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WILLOW SPRINGS WATER BANK CONJUNCTIVE USE PROJECT ELIGIBILITY A6 – OTHER
Eligibility, Section 3‐6, p.1
General Project Information Tab, Item A.6
Roadmap Attachment: Energy and GHG Benefits
Willow Springs Water Bank (WSWB) creates energy benefits and reduces Greenhouse Gas (GHG)
creation in California. The energy benefits are created from the incorporation of pumped storage into
the project and the development of a water/energy bank. The GHG reduction benefits result from onsite
renewables, shifting of water deliveries, and lack of methane creation in a surface reservoir. These are
non‐monetized benefits that clearly help California meet its renewable energy goals. They are detailed
as follows.
The energy and GHG benefits do not utilize any of the proposed WSIP grant funding. It will be paid for
independent of the Prop. 1 grant application process. The energy and GHG benefits are enabled by the
WSIP grant funding, but not part of it. WSIP funding is used exclusively for ecosystem and emergency
response benefits.
Pumped Storage
WSWB has evaluated the potential to develop hydropower through a California Energy Commission
(CEC) grant funded project (EPC‐15‐049). The CEC awarded WSWB a $197,000 grant to conduct the
evaluation. It was the highest ranked proposal among all submitted for this CEC solicitation. This
demonstrates the potential of a groundwater bank to harvest the benefits of the water/energy nexus.
The study found that about 5.2 MW of pumped storage hydropower could be generated onsite
economically. Additionally, about 27.3 MW of Demand Response capacity is possible using the same
facilities. This creates significant benefits for the California energy grid. The draft final report is located
in Appendix A.
The present worth of the combined onsite hydropower and demand response was estimated to be
about $8 M for WSWB. If WSWB is used as a template and extended to groundwater banks across the
state, the combination of hydropower and demand response has an annual value of about $ 6 M per
year.
Water/Energy Bank
WSWB has evaluated the potential to develop a water/energy bank through a California Energy
Commission (CEC) grant funded project (EPC‐16‐029) The CEC awarded WSWB a $1,000,000 grant to
conduct the evaluation. It was the highest ranked proposal among all submitted for this CEC solicitation.
This demonstrates the potential of a groundwater bank to harvest the benefits of the water/energy
nexus for demand response.
The water/energy bank will facilitate the shutdown of the Edmonston Pumping Plant during peak
summer hours, as well as the other 3 linked State Water Project pumping plants. These 4 pumping
plants are the largest single source of electric load in California. If the project is successful, up to 320
MW of Demand Response can be realized on average. This electric load will be shifted from a period of
electric shortage in the summer to a period of renewables surplus in the winter and spring. This is
accomplished through the creative use of water storage capacity. A summary of the ongoing study is
located in Appendix B.
WILLOW SPRINGS WATER BANK CONJUNCTIVE USE PROJECT ELIGIBILITY A6 – OTHER
Eligibility, Section 3‐6, p.2
The water/energy bank study is ongoing. One of the outcomes will be an estimated value of the Demand
Response benefits of the project. An order‐of‐magnitude estimate is included in the original proposal. It
shows that the avoided cost for a 320 MW combustion turbine is about $450 M. This will be refined as
the study develops. Because the water/energy bank relies on existing infrastructure plus the planned
WSWB, no significant additional capital facilities will be needed. As a result, the risk is all upside risk –
the benefit to California could be up to $450 M without any of the downside risk due to the cost of new
facilities.
GHG reductions
The GHG reduction benefits result from onsite renewables, shifting of water deliveries, and lack of
methane creation in a surface reservoir. Onsite solar is partially implemented. An expansion of onsite
solar is one of the areas of study in the CEC‐funded water/energy bank. GHG reductions due to a water
delivery shift will be confirmed in the ongoing CEC water/energy bank study. GHG reductions due to
avoidance of using surface water storage reservoirs is a new and emerging area of environmental
science. It is due to the creation of an anaerobic layer is surface reservoirs that contributes methane gas
to the atmosphere. Methane is a powerful GHG.
The use of groundwater storage at WSWB results in the following GHG reductions:
1. Reduced GHG due to the onsite solar energy = 140,000 metric tons per year (MT/yr.)
2. Reduced GHG due to the shift of water deliveries due to the water/energy bank = 94,000 MT/yr.
3. Reduced GHGs because WSWB is not a surface reservoir w/methane gas = 30,000 MT/yr.
4. Total GHG reduction = 264,000 MT/year, equivalent to taking 56,000 cars off the road.
This calculation is detailed Appendix C.
No estimate is made of the economic value of GHG reductions because it partially relies on avoided
action: it assumes surface reservoirs are not built. It also involves the construction of onsite renewable
energy facilities which may or may not prove to be economic. Consequently, it is another example of
positive risk which has little downside.
WILLOW SPRINGS WATER BANK CONJUNCTIVE USE PROJECT ELIGIBILITY A6 – OTHER APPENDIX
Appendix A
Energy Research and Development Division
FINAL PROJECT REPORT
Groundwater Bank Energy Storage Systems AFeasibilityStudyforWillowSpringsWaterBank
California Energy Commission Edmund G. Brown Jr., Governor
July 2017 | CEC-XXX-2017-XXX
PREPARED BY: Antelope Valley Water Storage, LLC
Primary Author(s):
Mark Beuhler
Naheed Iqbal
Zachary Ahinga
Contributor(s):
Lon W. House
Antelope Valley Water Storage, LLC
1672 W Avenue J Suite 207
Lancaster, CA 93534
Phone: 323-860-4824 | Fax: 661-945-4554
Contract Number: EPC-15-049
PREPARED FOR:
California Energy Commission
Yu Hou
Project Manager
Aleecia Gutierrez
Office Manager
ENERGY GENERATION RESEARCH OFFICE
Laurie ten Hope
Deputy Director
ENERGY RESEARCH AND DEVELOPMENT DIVISION
Robert P. Oglesby
Executive Director
DISCLAIMER
This report was prepared as the result of work sponsored by the California Energy Commission. It does
not necessarily represent the views of the Energy Commission, its employees or the State of California.
The Energy Commission, the State of California, its employees, contractors and subcontractors make no
warranty, express or implied, and assume no legal liability for the information in this report; nor does any
party represent that the uses of this information will not infringe upon privately owned rights. This report
has not been approved or disapproved by the California Energy Commission nor has the California Energy
Commission passed upon the accuracy or adequacy of the information in this report.
i
ACKNOWLEDGEMENTS
The authors wish to thank the following individuals and organizations for their support
towards the completion of this study:
Technical Advisory Committee members: Adam Hutchinson (Orange County Water District
(OCWD)), Ted Johnson (Water Replenishment District of Southern California (WRD)), Garry
Maurath (California Energy Commission), and Robert Wilkinson (University of California, Santa
Barbara)
Yu Hou (California Energy Commission)
Tommy Ta (Antelope Valley Water Storage, LLC)
Will Boschman of the Semitropic-Rosamond Water Bank Authority for selected photographs
Subcontractor firm: HDR Engineering, Inc. (HDR)
The agencies that responded to the survey: Castaic Lake Water Agency (CLWA); City of
Bakersfield, Water Resources Department; Elsinore Valley Municipal Water District; Foothill
Municipal Water District; James Irrigation District; Mojave Water Agency; Monterey Peninsula
Water Management District; Orange County Water District; Root Creek Water District; Rosedale-
Rio Bravo Water Storage District; San Bernardino Valley Water Conservation District; Three
Valleys Municipal Water District; United Water Conservation District; and Western Municipal
Water District
ii
PREFACE
The California Energy Commission’s Energy Research and Development Division supports
energy research and development programs to spur innovation in energy efficiency, renewable
energy and advanced clean generation, energy-related environmental protection, energy
transmission and distribution and transportation.
In 2012, the Electric Program Investment Charge (EPIC) was established by the California Public
Utilities Commission to fund public investments in research to create and advance new energy
solution, foster regional innovation and bring ideas from the lab to the marketplace. The
California Energy Commission and the state’s three largest investor-owned utilities – Pacific Gas
and Electric Company, San Diego Gas & Electric Company and Southern California Edison
Company – were selected to administer the EPIC funds and advance novel technologies, tools,
and strategies that provide benefits to their electric ratepayers.
The Energy Commission is committed to ensuring public participation in its research and
development programs that promote greater reliability, lower costs, and increase safety for the
California electric ratepayer and include:
• Providing societal benefits.
• Reducing greenhouse gas emission in the electricity sector at the lowest possible cost.
• Supporting California’s loading order to meet energy needs first with energy efficiency
and demand response, next with renewable energy (distributed generation and utility
scale), and finally with clean, conventional electricity supply.
• Supporting low-emission vehicles and transportation.
• Providing economic development.
• Using ratepayer funds efficiently.
Groundwater Bank Energy Storage Systems:A Feasibility Study for Willow Springs Water Bank is
the final report for the Electricity Pumped Storage Systems using Underground Reservoirs: A
Feasibility Study for the Antelope Valley Water Storage System project (Contract Number EPC-
15-049, Grant Number GFO-15-309) conducted by Antelope Valley Water Storage, LLC. The
information from this project contributes to Energy Research and Development Division’s EPIC
Program.
All figures and tables are the work of the author(s) for this project unless otherwise cited or
credited.
For more information about the Energy Research and Development Division, please visit the
Energy Commission’s website at www.energy.ca.gov/research/ or contact the Energy
Commission at 916-327-1551.
iii
ABSTRACT
Increased renewable generation in California has resulted in an excess of electricity supply
during afternoon hours. Energy storage systems make it possible to repurpose the supply glut
to meet grid needs during evening hours and thereby, help with integration of renewable energy
into the electric grid. Pumped storage is a well-established type of energy storage which uses
water to store energy during the off-peak (low demand) hours. The stored energy is released
during the dusk hours when there is a spike in electricity demand. Integrating pumped storage
with groundwater banking operations has the potential to increase the number and type of
areas where pumped storage can be implemented. The objective of this study is to address the
knowledge gaps associated with having onsite pumped storage at groundwater banks. The
study evaluated two pumped storage systems: Peak Hour Pumped Storage (PHPS), that has all
the components aboveground, and Aquifer Pumped Hydro (APH), that uses the aquifer as the
lower reservoir. Besides pumped storage, hydropower generation and demand response
potential of groundwater banking projects were also assessed. The hydrologic year type will
determine which of the three configurations is used in a particular year. These configurations
and their corresponding economic values were analyzed for an existing groundwater banking
project, Willow Springs Water Bank (WSWB) which served as a case study for this project. The
WSWB specific findings we use to evaluate the potential of statewide implementation of PHPS
and APH. The analysis shows that the demand response during a dry hydrologic year has the
highest value. To enhance the economic viability of energy storage systems as well as to
address the grid needs, the groundwater bank should be configured to provide demand
response during a dry year as well as hydropower generation, demand response, and pumped
storage benefits in other hydrologic year types.
Keywords: California Energy Commission, pumped storage, groundwater banks, energy storage
systems, demand response, hydropower generation, renewable energy
Please use the following citation for this report:
Beuhler, Mark, Naheed Iqbal, Zachary Ahinga, and Lon W. House. Antelope Valley Water Storage,
LLC. 2017. Groundwater Bank Energy Storage Systems: A Feasibility Study for Willow
Springs Water Bank. California Energy Commission. Publication Number: CEC-XXX-2017-
XXX.
iv
v
TABLE OF CONTENTS
Page
ACKNOWLEDGEMENTS i
PREFACE ii
ABSTRACT iii
TABLE OF CONTENTS v
LIST OF FIGURES viii
LIST OF TABLES ix
EXECUTIVE SUMMARY 1
Introduction 1
Project Purpose and Description 1
Project Process 2
Project Results 4
Benefits to California 4
CHAPTER 1: Introduction 7
1.1 Background 7
1.2 Objectives 9
1.3 Energy Storage Systems at Groundwater Banks 10
1.3.1 Willow Springs Water Bank 11
CHAPTER 2: Aquifer Pumped Hydro at Willow Springs Water Bank 12
2.1 Key Parameters for Power Generation 16
2.2 Round Trip-Efficiency and Head Loss Effects 17
2.2.1 WSWB Site - Aquifer Pumped Hydro Round-Trip Efficiency 17
2.2.2 Head Loss Due to Drawdown and Mounding 20
2.2.3 Key Finding 22
2.3 Power Generation for a Single APH Turbine Setup 25
2.4 Cost Estimates 25
2.5 State Water Resources Control Board (SWRCB) Regulations 27
2.5.1 Short Term Pilot Test 28
2.5.2 Long Term Projects 28
2.6 Demand Response Potential of the Well Field 28
vi
2.6.1 Automated Remote Control of the Well Field System 29
CHAPTER 3: Peak Hour Pumped Storage at Willow Springs Water Bank 31
3.1 Operating Scenarios 32
3.2 Components and Factors for Peak Hour Pumped Storage 33
3.2.1 Reservoir Site Analysis 33
3.2.2 Selection of Generator Type 36
3.2.3 Total Energy Losses 38
3.3 Calculation of Hydropower Generation 38
3.4 Extended Duration Battery Potential 39
3.5 Demand Response Potential of the Pumping Plant 40
3.6 Cost Estimates 40
3.7 CEQA Considerations 41
3.8 Summary of WSWB Pumped Storage Analysis 42
CHAPTER 4: Statewide Applicability Analysis 45
4.1 Literature Review and Statewide Survey 45
4.2 Analysis Approach for Peak Hour Pumped Storage 46
4.2.1 Statewide PHPS Potential at Groundwater Banking Projects 47
4.3 Aquifer Pumped Hydro Potential 50
4.3.1 Aquifer Storage and Recovery (ASR) Projects 50
4.3.2 Recycled Water for Direct Injection 51
4.4 Demand Response Potential of Groundwater Banks 54
4.4.1 Peak Energy Requirements at Groundwater Banks 55
4.4.2 Demand Response Potential associated with Well Pumps 55
4.4.3 Demand Response Potential associated with Pump Station(s) 58
4.5 Regulatory Considerations 58
4.6 Template to Assess Pumped Storage Potential 59
4.7 Summary of Statewide Analysis 59
CHAPTER 5: Economics Evaluation 62
5.1 Participation in ISO Markets 62
5.1.1 Day-Ahead market 62
5.1.2 Real-time market 62
5.1.3 Ancillary service market 63
vii
5.1.4 Load Participation 63
5.1.5 Other Markets/Services 64
5.2 Economics Analysis Approach 67
5.3 Economic Feasibility at Willow Springs Water Bank 67
5.3.1 Operating Scenarios 67
5.3.2 StorageVET™ Model 69
5.3.3 Aquifer Pumped Hydro (APH) Economics 69
5.3.4 Peak Hour Pumped Storage (PHPS) Economics 71
5.3.5 Dry Year (35% probability) – Demand Response 73
5.4 Economic Evaluation for Statewide Pumped Storage at Groundwater Banks 77
5.4.1 Potential Markets and Services 77
5.4.2 Statewide Potential from Adding Pumped Storage to Groundwater Banks 81
CHAPTER 6: Project Benefits 83
6.1 Addressing the Duck Curve Problem 83
6.1.1 Wet Hydrologic Year 85
6.1.2 Neutral Hydrologic Year 85
6.1.3 Dry Hydrologic Year 86
6.2 Greenhouse Gas (GHG) Emissions Reduction 87
CHAPTER 7: Results and Conclusions 88
GLOSSARY 90
References 91
APPENDIX A: Sensitivity Analysis A-1
Equations Utilized A-1
Results A-2
APPENDIX B: Field Measurement of Well Startup & Shutdown Time Durations B-1
Test Protocol B-1
Field Data B-1
APPENDIX C: WSWB Upper and Lower Reservoir Site Maps C-1
APPENDIX D: Statewide Survey Results D-1
Statewide Survey Responses D-1
APPENDIX E: Small Hydropower Potential for Groundwater Banking Agencies E-1
viii
APPENDIX F: Well Pumps Demand Response Potential for Selected Groundwater Banking
Projects F-1
APPENDIX G: List of Required Permits and Registrations G-1
ATTACHMENT I: Willow Springs Water Bank (WSWB) Fact Sheet I
LIST OF FIGURES
Page
Figure 1: Recharge Basins at a Typical Groundwater Banking Project .................................................. 8
Figure 2: An individual unit of the APH pumped hydroelectric system ............................................ 13
Figure 3: An APH unit in generating and storing modes ...................................................................... 14
Figure 4: Interaction of APH unit with the electrical grid ..................................................................... 15
Figure 5: APH modules within the well array .......................................................................................... 16
Figure 6: Pump Test Data for WSWB Well AV-2 ...................................................................................... 18
Figure 7: Pump Test Data for WSWB Well AV-5 ...................................................................................... 19
Figure 8: Pump Test Data for WSWB Well AV-3 ...................................................................................... 19
Figure 9: WSWB Hydropower Generation Operations ............................................................................ 32
Figure 10: Potential Upper and Lower Reservoir Sites ........................................................................... 34
Figure 11: Francis Turbine ........................................................................................................................... 36
Figure 12: 5-Jet Pelton Wheel Impulse Turbine (Elevation and Plan Views) ...................................... 37
Figure 13: A Groundwater Well at Willow Springs Water Bank ............................................................ 43
Figure 14: Monthly Groundwater Production (taf) by Hydrologic Region and Type of Use .......... 57
Figure 15: Operating Configurations for WSWB by Year Type ............................................................. 68
Figure 16: Renewable Energy Generation, April 27, 2017 ..................................................................... 83
Figure 17: California ISO “Duck Curve” .................................................................................................... 84
Figure 18: WSWB PHPS Hypothetical Operation During Wet Year ...................................................... 85
Figure 19: WSWB PHPS Hypothetical Operation During Neutral Year ................................................ 86
Figure 20: WSWB Hypothetical Operation During Dry Year ................................................................. 86
ix
LIST OF TABLES
Page
Table 1: Summary of Pump Test Data for WSWB Wells AV-2, AV-3 and AV-5 ................................. 18
Table 2: Summary of Drawdown Efficiency ............................................................................................. 21
Table 3: Target Average Efficiency of Aquifer Pumped Hydro Energy Storage ............................... 22
Table 4: Energy Storage Efficiency and Costs .......................................................................................... 22
Table 5: Power Calculation for One “Pump As Turbine” Setup at WSWB .......................................... 24
Table 6: Potential Power Generation for Well AV-5 at WSWB ............................................................... 25
Table 7: Capital Cost of Facilities for One Aquifer Pumped Hydro Unit ........................................... 26
Table 8: Costs to generate hydropower using existing wells at WSWB .............................................. 27
Table 9: Cost to Install one XiO Field Installed Well Control Unit ...................................................... 30
Table 10: Summary of Potential Land for Upper Reservoir .................................................................. 35
Table 11: Summary of Potential Land for Lower Reservoir .................................................................. 36
Table 12: Reservoir, Generator, and Pump Power Calculations ........................................................... 38
Table 13: Summary of Upper and Lower Reservoir Sizing ................................................................... 39
Table 14: Capital Cost of Facilities for PHPS and Demand Response ................................................ 41
Table 15: Power Generation and Demand Response Potential at WSWB ........................................... 42
Table 16: Peak Hour Pumped Storage (PHPS) potential at Groundwater Banking Projects ........... 50
Table 17: Projects Using Recycled Water for Groundwater Recharge Via Injection ........................ 52
Table 18: Planned Projects Using Recycled Water for Groundwater Recharge Via Injection ........ 53
Table 19: Demand Response Potential of Well Pumps at Groundwater Banking Projects ............ 58
Table 20: Storage Reliability Services and Non-Reliability Services .................................................... 64
Table 21: Potential Markets and Services for Groundwater Bank Pumped Storage Operation .... 65
Table 22: StorageVET™ Technology Parameters Used for WSWB APH Simulation ......................... 70
Table 23: Economics of APH Operation at WSWB ................................................................................... 70
Table 24: StorageVET™ Technology Parameters Used for WSWB PHPS Simulation ........................ 71
Table 25: WSWB PHPS Operation (Neutral Year – 33% Probability) ..................................................... 72
Table 26: WSWB Hydroelectric Generator Mode (Wet Year – 32% Probability) ................................. 72
Table 27: Cost effectiveness of PHPS and Hydropower Generation at WSWB .................................. 73
Table 28: Types of Demand Response ...................................................................................................... 74
Table 29: WSWB Operated as a Continuous Load (Dry Year – 35% Probability) ............................... 75
x
Table 30: Comparison of WSWB APH and PHPS Characteristics and Analysis ................................ 75
Table 31: Potential Markets for Groundwater Bank Energy Operations ............................................ 78
Table 32: Statewide Potential, Benefits, and Costs of Pumped Storage at Groundwater Banks ... 81
Table 33: Annual GHG Emissions Reduction from PHPS at Groundwater Banks ............................ 87
1
EXECUTIVE SUMMARY
Introduction
California is experiencing a surge in renewable generation that has resulted in operational
challenges for the grid. Solar generators comprise majority of the renewable energy and their
output varies throughout the day. This is causing a mismatch between energy supply and
demand, with a glut of supply in the afternoon hours (when the solar generation peaks) and a
shortage of supply in the evening hours (when the renewable generation ceases for the day).
This mismatch is represented by a daily electric demand curve (“duck curve”) that dips in
afternoon and rises sharply in evening and resembles the profile of a duck. To address this
mismatch and move the excess energy from periods of low demand to periods of high demand,
the electric grid must have energy storage systems.
Pumped storage is an established energy storage technology and has been deployed nationwide.
It works by pumping water from a lower reservoir to a higher one. Energy is stored in the form
of gravitational potential energy of water. Electricity is generated when the stored water at the
higher elevation returns to the lower reservoir through a turbine generator.
Project Purpose and Description
The purpose of this project is to evaluate the feasibility of using the conventional pumped
storage concept in a novel way to provide cost-effective and reliable energy storage. The State is
home to a number of groundwater banking facilities that safeguard against potential water
shortages (such as the ones occurring during the recent 2013—2015 drought). The project
examines the applicability of implementing pumping storage at these groundwater banks. The
banks store water in the natural underground reservoirs (aquifers) in wet years and pump it out
for use in dry years via groundwater wells. The primary function of these banks is water
storage and there is no precedent for evaluating these banks for pumped storage. These sites
present an opportunity for pumped storage systems because they have water supplies and an
existing infrastructure (including wells and pipelines) to cycle the water for energy storage.
Therefore, pumped storage implementation at these sites requires minimal additional facilities
and has a smaller environmental footprint than that of conventional pumped storage.
The project evaluates two pumped storage technologies: Peak Hour Pumped Storage (PHPS) and
Aquifer Pumped Hydro (APH) for their applicability at groundwater banks. Conceptually, PHPS
operates like the conventional pumped storage – water is cycled between two surface reservoirs
through a connecting pipe to store and release energy. However, PHPS is much smaller in scale
and can be implemented in areas that would normally be precluded from consideration for
conventional pumped storage. An APH unit uses the aquifer as a lower reservoir in conjunction
with a surface (upper) reservoir. A groundwater well cycles the water between the two
reservoirs. It is a novel form of pumped storage and has been the subject of only a few studies.
2
Project Process
A two-fold approach was adopted for the analysis. The PHPS and APH potential was first
determined for an existing groundwater banking project, Willow Springs Water Bank (variously
referred to as “the Bank” or WSWB in this report). The WSWB specific analysis yielded criteria
which the project team used to evaluate other sites and develop an estimate of cumulative
pumped storage capacity (MW) available at statewide groundwater banks.
WSWB has a 5.2 MW capacity for PHPS. The PHPS facility at WSWB can generate energy up to 12
hours daily depending on the size of the upper reservoir. During the remaining hours, water is
pumped to the upper reservoir to refill it. Statewide, the cumulative PHPS potential is estimated
to be 44 MW. APH is infeasible at WSWB because of low round-trip efficiency. Preliminary
screening of other sites indicates that the APH has limited statewide potential.
Economics Evaluation
Just as water storage infrastructure at groundwater banks can be used for energy storage, the
pumped storage facilities at groundwater banks can be used to provide energy benefits other
than energy storage. These benefits include hydropower generation (water passing through the
turbines to generate energy without first being pumped to an upper reservoir) and demand
response (changing load or demand based on grid requirements). Which of the energy benefits
occur at any one time is determined by the hydrologic year type which in turn determines the
operating mode for the groundwater banking facilities (including any installed pumped storage
facilities). These additional benefits were taken into consideration when evaluating the
economic feasibility of pumped storage at groundwater banks.
The operations of a typical groundwater banking project such as WSWB vary based on the
hydrological year type. During neutral or idle year type the water bank is neither recharging nor
extracting water. During a wet year type the water bank is continuously recharging water.
During dry years the water bank is continuously extracting water.
For economic evaluation, an operating mode configuration was assigned to each of these year
types:
In a neutral year, the Bank was assessed as a pumped storage facility which uses APH or PHPS
technology to generate when electricity prices are high, and refill storage when prices are low.
Because of the low response time and round-trip efficiency APH at WSWB was found to be
suited for only for one electricity market.
In a wet year, the Bank was assessed as a generator which uses turbines (same turbines as used
for PHPS in a neutral year) to generate 5.2 MW constantly over the year. The well field cannot
similarly be used for generating hydropower in a wet year because this requires the recharge
water to be injected into the ground instead of percolated. Using injection wells will incur
additional costs which makes well field dependent hydropower generation impractical.
In a dry year the Bank pumps the stored water and has pumping demand from groundwater
wells (17.2 MW) and the pump station (10.1 MW). In this year, the Bank acts as a continuous
3
load and can be configured for demand response that is the wells and pump station can be
turned off during the on-peak (high electricity demand) periods.
The table below summarizes the operational configurations for WSWB that use existing water
banking facilities in conjunction with additional facilities installed for PHPS and APH to provide
pumped storage, demand response and hydropower generation.
WSWB PHPS and APH Operating Scenarios
Hydrologic Year Type
Probability of Occurrence
WSWB Operation
Type
Electricity Demand Potential
Electricity Generation Potential
Evaluated As
APH
Wet 32% Recharge 0 0
Neutral 33% Idle 17.2 MW 3.7 MW for 5 hours daily
Pumped Storage
Dry 35% Extraction 17.2 MW groundwater
pumping + 10.1 MW pump station
use
0 Demand Response
PHPS
Wet 32% Recharge 0 5.2 MW 24 hours daily
Generator
Neutral 33% Idle 10.1 MW pump station use
5.2 MW for 5 hours daily
Pumped Storage
Dry 35% Extraction 17.2 MW groundwater
pumping + 10.1 MW pump station
use
0 Demand Response (demand reduction)
Source: (House L. W., 2017 a)
The estimated statewide pumped storage and demand response potential was used in
conjunction with the operating configurations developed for WSWB to evaluate the value of
pumped storage and associated benefits at other groundwater banks. This approach assumes
that WSWB operations are representative of typical groundwater banking projects. Therefore, all
the groundwater banking projects in the State (including WSWB) have an estimated 44 MW of
cumulative PHPS potential (in a neutral year), 44 MW of cumulative hydropower generation
potential (in a wet year), limited cumulative APH potential (in a neutral year), and 220 MW of
cumulative demand response potential (in a dry year).
4
Project Results
PHPS facilities, if configured appropriately, can be potentially economically viable but an APH
setup is unlikely to be so at typical groundwater banking projects. The net present value (NPV)
method was used to evaluate costs and revenues for PHPS and APH. A positive NPV indicates
that a project is financially viable. Projects with negative NPV should generally be avoided. The
results show that adding dry year demand response to a PHPS facility’s wet and neutral year
operations makes it cost effective but adding dry year demand response to APH is not enough
to make APH cost effective. The table below summarizes these findings:
Comparison of WSWB APH and PHPS Operational Analysis
Aquifer Pumped Hydro (APH)
Peak Hour Pumped Storage (PHPS)
Demand Response
Components needed
Reversible pump-turbines, surface storage reservoir, aquifer lower
reservoir
Hydroelectric generator, upper and lower surface
reservoirs
Additional groundwater wells for 320 hours
curtailment
Capital Cost $18.6M $7.9M $2.1MNet Present Value (NPV)
-$18.2M (generator operating in neutral
years)
-$0.9M (generator operating during wet and
neutral years)
$9.1M (dry years)
Capital Cost with Dry Year Demand Response
$20.3M $10M -
Net Present Value (NPV) with Dry Year Demand response
-$9.1M $8.1M -
Source: (House L. W., 2017 a)
44 MW of statewide PHPS potential (with PHPS facility used for both pumped storage and
hydropower generation and evaluated with dry year demand response) has an annual net
benefit of $5.9 M and the 220 MW of statewide load used for demand response purposes has an
annual net benefit of $6.3 M.
Benefits to California
Energy storage is one of the solutions being explored to address the “duck curve” problem. This
problem is projected to worsen as more renewables come online and is characterized by an
excess of generation during the afternoon hours (when solar generation peaks), a very steep
ramp in generation requirement during the late afternoon (as solar generation ends), followed
by a peak generation requirement during the evening. The analysis shows that the PHPS
facilities at groundwater banks can be economically viable if appropriately configured and have
the potential to mitigate the duck curve problem by:
Curtailing hydropower generation during afternoon (renewable overproduction period) in a
wet hydrologic year.
5
Generating hydropower during the morning and evening ramp periods, and increasing
demand (pumping load) to refill reservoirs during the afternoon (renewable
overproduction period) in a neutral hydrologic year.
Curtailing pumping load during the late afternoon ramping period and evening peak in a
dry hydrologic year.
Besides enabling renewable integration, implementing pumped storage facilities at groundwater
banks also benefits California by adding to the renewable generation capacity, and providing
demand response benefits that can help out the grid in the event of unplanned outages.
Pumped storage facilities at groundwater banks can also enable participation in additional
electricity markets to provide more services provided the facilities are configured properly and
the water banks are willing to turn over operational control of the facilities to the Independent
System Operation (that is to an entity that manages the electricity flow and operates the electric
grid). Using small scale pumped storage also decreases the need for large, environmentally
invasive new reservoirs thus reducing the risk of catastrophic floods after an earthquake. The
statewide PHPS potential of 44 MW is expected to address up to 1% of the State’s storage needs
and results in an annual greenhouse gas emissions reduction of 44,000 metric tons of carbon
dioxide equivalent (CO2e) GHG reductions on average. An extensive database of statewide
groundwater banking facilities was compiled for this project. The project team has also
developed PHPS and APH templates which together with the database can be used to identify
potential sites for testing the pumped storage concepts in a next-step pilot project. Particularly
favorable sites include groundwater banks in the Tulare Basin and in the Southern California
coastal plain, where both the pumped storage and the demand response aspects can be
exploited.
6
7
CHAPTER 1: Introduction
Groundwater banks are underground storage facilities that are used for banking or storing
water. Stored water can be recycled water, imported water from other areas (typically Northern
California) or local surface water. In addition to their primary function of water storage,
groundwater banks also provide an opportunity to store energy. Harnessing the potential of
water for energy storage purposes is not new. Conventional water storage or pumped storage is
a well-established technology with multiple projects in California. In contrast, pumped storage
using a groundwater bank and the aquifer is far from established. This Electric Program
Investment Charge (EPIC) funded project assesses the statewide pumped storage potential of
groundwater banks and provides a framework to utilize groundwater banks for cost-effective
and efficient distributed energy storage. The study investigates two different kinds of pumped
storage. The first one called Peak Hour Pumped Storage (PHPS) is similar to the conventional
pumped storage with the difference being that instead of building new dedicated facilities
including large surface reservoirs, existing groundwater banking facilities can be modified and
enhanced with hydroelectric generators and surface storage reservoirs to cycle water with a
much smaller environmental footprint. The second one called Aquifer Pumped Hydro (APH)
uses the aquifer below a groundwater bank as the lower reservoir, a small earthen reservoir as
the upper reservoir and reversible pump turbine groundwater wells (instead of a pipeline) to
cycle the water.
1.1 Background The increased renewable generation in California has made integrating renewables into the grid
a top priority. Energy storage systems are necessary to allow for smooth integration of
renewables such as wind and solar and to overcome the “duck curve” problem. The duck curve
problem is an imbalance in supply and demand at various times of the day resulting from the
nature of the renewables (particularly solar). Since renewables are generating energy mostly
during the afternoon hours, there is overgeneration during the day. By evening as solar
generation peters out, the demand ramps up. Consequently, the daily net electric demand (total
demand for electricity net the renewable generation) change considerably throughout the
course of a day. This is reflected in a duck shaped profile (duck curve) for the net electric
demand with the belly of the duck representing the glut of energy (low net demand) and the
head representing the shortage (high net demand).
Without adequate storage, the duck curve problem is projected to be exacerbated as more
renewable sources come online to meet the State of California’s target of 50% renewable
electricity by 2030 and the potential goal of 100% by 2045 (Senate Bill 100). The capability to
provide peak electricity during the early evening as solar generation ramps down will become
increasingly important. Consequently, various storage technologies are being explored and
developed to provide reliable and cost-effective storage. Conventional pumped hydroelectric
8
storage has been the dominant energy storage technology in the United States and has been
widely deployed all over the country and globally to provide peak hour energy and to increase
grid reliability and flexibility. The conventional form of pumped storage uses two reservoirs
(usually a dam and an aqueduct) situated at different elevations to cycle the water. Water is
pumped to the higher elevation reservoir during off-peak hours to store energy. During on-peak
hours, water flows by gravity to the lower reservoir generating energy in the process. This
technology is limited by topography, environmental concerns, high cost, and the large size
requirements needed to make it practical. Most of the best sites for surface reservoirs have
already been taken limiting the wider use of pumped storage.
Groundwater banks (Figure 1) offer an opportunity to expand the geographic scope of pumped
storage. As traditional pumped storage, pumped storage at groundwater banks has the
potential to store excess energy during non-peak hours for release during the dusk (peak) hours
when the grid needs it the most. Using groundwater banks for pumped storage operations will
also have fewer environmental impacts including reduced risk of catastrophic flooding.
Figure 1: Recharge Basins at a Typical Groundwater Banking Project
Figure 1 shows recharge activities via spreading at Semitropic Groundwater Storage Bank in Central Valley, California.
Although groundwater banks have traditionally been used only for water storage, they may have potential as energy
storage systems as well.
Source: (Semitropic Water Storage District, 2017)
Unlike traditional pumped storage, the use of pumped storage in conjunction with a
groundwater bank remains largely unexplored. This study is the first of its kind to put forward
a conceptual framework to assess the potential of pumped storage at groundwater banks in
9
California. It identifies and analyzes current policy, regulatory, economic and technical
parameters pertinent to the implementation of pumped storage operations at existing and
planned groundwater banks to determine value of the PHPS and APH energy storage system
technologies. The value of these technologies lies in their role as ‘transition’ energy storage
systems—they will start up when the quick response (seconds) but low capacity energy storage
(battery/flywheels) runs out and before slow response (minutes or hours) but high capacity
storage (large pumped hydro facilities) engages. Statewide application of pumped storage at
groundwater banks has the potential to enhance grid reliability by enabling greater integration
of solar and wind energy and providing power during unplanned outages.
The study establishes the potential of pumped storage at an existing large groundwater bank in
the Antelope Valley, Willow Springs Water Bank (variously referred to as “the Bank” or WSWB in
this report) and identifies criteria thresholds that must be met for the successful deployment of
the two ESSs at other groundwater banks. This information is then used to provide estimates of
statewide potential, taking into consideration specific characteristics of other regions and other
groundwater banking projects. The statewide potential is evaluated in context of the State’s
storage needs with description of major limitations and anticipated costs and benefits.
1.2 Objectives The study evaluates the energy storage potential of groundwater banks, specifically (1)
potential of Peak Hour Pumped Storage (PHPS) technology which uses surface reservoirs at
groundwater banks; and (2) potential of Aquifer Pumped Hydro (APH) technology which uses
the aquifer at groundwater banks (APH). The study has three objectives:
Feasibility analysis of PHPS and APH technologies at WSWB including development of
optimized facilities layout for the two energy storage systems (ESSs)
Assessment of statewide potential of the pumped storage at groundwater banks including
identification of criteria and specific groundwater banking sites or regions where the
two technologies are likely to be successful
Estimation of the value of energy storage and other grid benefits provided by the two
technologies.
The key features of the study include (1) analyzing the impact of various storage capacities on
the duration of energy release, (2) developing an optimized layout containing specifications for
reservoirs, generators, and locations along with the corresponding peak power generation
potential in MW, (3) creating a template that can be used to determine the groundwater banking
areas where energy storage and peak power generation is practical, and (4) providing initial
estimates of peak energy generation and associated grid support benefits resulting from
pumped storage at groundwater banks. Ultimately, the goal of the study is to provide a
preliminary assessment of the statewide potential for pumped storage systems at groundwater
banking projects.
10
1.3 Energy Storage Systems at Groundwater Banks Groundwater banks have not traditionally been targeted to provide peak energy. Currently,
there are more than 90 groundwater banking projects spread across California (Antelope Valley
Water Storage (AVWS), 2016). Many new groundwater banking operations and recycled water
programs are planned to be implemented as a result of the Water Quality, Supply, and
Infrastructure Improvement Act of 2014 (Proposition 1) and Sustainable Groundwater
Management Act (SGMA). This study evaluates the potential of two as yet untested pumped
storage technologies at groundwater banks. The PHPS technology uses a combined
pump/generator pumping station in conjunction with an upstream surface reservoir and a
downstream surface reservoir. PHPS is best suited for groundwater banks that have elevational
differences within their groundwater bank and suitable surface area to construct additional
surface storage reservoirs. The elevation difference between the reservoirs provides the
pumping lift and the reservoirs are connected by a pipe. Energy is generated when the water
flows to the lower reservoir during peak hours when the electricity demand is high. During non-
peak hours energy is stored by transporting water to the upper reservoir. Depending on the
size of the reservoirs and the pumping lift involved, a PHPS project can discharge energy over a
long duration or during the peak hours and allows rapid demand management. Although
relatively proven, PHPS is a novel concept in the context of being implemented at a
groundwater bank for daily peaking.
APH is an underground pumped hydroelectric energy storage method that uses aquifer as the
lower reservoir of a pumped hydro system. An APH unit consists of a reversible pump/turbine,
a well, and related equipment. The pump/turbine generates electricity from water flowing down
the well hole. It stores electricity at other times by pumping water up the well to a surface
reservoir using electric power. APH is best suited for groundwater banks that have aquifers
with high groundwater transmissivity, deep water levels, and surplus well capacity. APH can be
implemented as a modular array to capture electrical oversupply, store electrical energy and
provide distributed generation and demand response. Most of the studies of underground
pumped hydro concept date back to 1970’s and 1980’s1 and focus on using a large
underground cavern, either available from abandoned mines or excavated, as the lower
reservoir. Energy storage needs has caused a resurgence of interest in the underground
pumped hydroelectric energy storage method and largescale utility sized projects (1,000-3,000
MW) using underground caverns have been evaluated in recent years (Fairley, 2015; Madlener,
2013; Uddin & Asce, 2003; Tam, Blomquist, & Kartsounes, 2007; Pickard, 2012). While none of
these largescale projects have been built, there are existing permits at the Federal Energy
Regulatory Commission for some of these projects2. The concept of using the aquifer, rather
than an underground cavity, as the lower reservoir has been explored by very few studies
1 (Allen, Doherty, & Kannberg, 1984; Blomquist C. , Frigo, Tam, & Clinch, 1979; Braat, van Lohuizen, & de Haan, 1985; Chang, Thompson, Allen, Ferreira, & Blomquist, 1980; Doherty, 1982; Farquhar, 1982; Frigo, Blomquist, & Degnan, 1979; Blomquist, Frigo, & Degnan, 1979; Frigo & Pistner, 1980; Ridgway, Dooley, & Hammond, 1979) (Rogers & Larson, 1974) (Rogers F. C., 1975) (Scott, 2007) (Willett & Warnock, 1983)
2 For example, FERC Project No. 14612-000, New Summit Hydro LLC, is for 1,500 MW pumped hydro storage project in Ohio using an abandoned underground limestone mine as the lower reservoir.
11
(Martin, 2007; S.Y. & I.E., 2017; Budris, 2014) and these evaluations have been of a preliminary
nature.
This study uses data from an operating groundwater bank to study the APH in more depth and
provides valuable information about the efficiency, costs and value estimates for the APH form
of pumped storage. The study also assesses potential use of recycled water for APH to
eliminate ½ of the round trip and improve the overall efficiency of peak hour power generation.
Discuss results rather than listing them.
1.3.1 Willow Springs Water Bank
Willow Springs Water Bank (WSWB) is a groundwater banking project located in Antelope Valley,
California on approximately 1,838 acres of agricultural land. The Bank has 500,000 acre-feet
(AF) of approved storage capacity. Recent groundwater modeling results indicate that the
Bank’s capacity can be increased to 1,000,000 AF. Additional details about WSWB are provided
in the WSWB Fact Sheet (Attachment I).
At WSWB, the pumping lifts are 350’ to 450’ for the PHPS and APH energy storage systems. The
Bank’s build out plan also includes a big pipe, a pump station/turbine, and potential sites for
large upstream and downstream reservoirs. Therefore, WSWB provides a good opportunity for
preliminary assessment of pumped storage potential at groundwater banks.
The study uses design information for the Bank’s facilities, water quality and aquifer data, and
well drawdown results to provide conclusions about the economic and technical feasibility of
the two pumped storage technologies at WSWB. The optimized facility layout for PHPS
technology was developed as part of the study. This layout balances various parameters such as
size of the generating equipment, discharge duration and reservoir capacity to achieve a PHPS
configuration that integrates well with the WSWB operations and maximizes the benefits to the
grid in a cost-effective way. Existing wells at WSWB were used for field evaluation of the
startup and shutdown times.
The findings from the WSWB site specific analysis were used to develop criteria to evaluate
pumped storage potential at other groundwater banks.
12
CHAPTER 2: Aquifer Pumped Hydro at Willow Springs Water Bank
This chapter describes the technical feasibility of Aquifer Pumped Hydro (APH) at Willow
Springs Water Bank (WSWB). APH uses the existing groundwater aquifer as a lower reservoir and
a surface reservoir as the upper reservoir. The existing electric grid provides the energy source
and sink. The system operates on a cycle that has two stages – storage and generation. During
the storage stage water is pumped out of the groundwater aquifer into the upper reservoir, and
during the generation stage, water is injected back into the groundwater aquifer via the
pump/turbine generator and well shaft piping. APH has to be installed so as not to interfere
with the primary operations of a groundwater bank and uses wells that are part of the
groundwater bank.
The study examined the potential of Aquifer Pumped Hydro (APH) to produce hydropower
during the 5 peak hours of the day. An APH unit consists of an existing WSWB well, piping, and
reservoir facilities. A typical well at WSWB includes a 300 HP 480 Vac (Volts, alternating
current) 3-wire electric pump motor, standard centrifugal vertical-turbine pump, motor control
panels, electrical panels, circuit breakers and transformer unit. The vertical-turbine pump is
operated in the forward direction using electric power to pump water and would be operated in
the reverse direction, “Pump As Turbine” to generate electric power.
To enable the pump to operate in the reverse direction to generate electric power, required
modifications to the system may include:
1. Pump shaft modification to enable the shaft to turn in the reverse direction.
2. Addition of pressure control valve on pump shaft and electronic valve control unit.
3. Addition of Power Electronics Controller to excite the motor-generator and rectify the
output to enable motor to operate efficiently as a generator.
4. Addition of a grid-tie inverter/rectifier.
5. Addition of System Control and Monitoring for overall control and protection of all the
elements of the electrical system, with primary job to route power to and from the energy
storage system, local power sources and the loads.
6. Modification of electric system to interface with energy sources, user loads, and utility grid.
Providing detailed designs of these modifications is not part of this study and should be part of
a next-step pilot-program to confirm the appropriate component size/capacity and
effectiveness of the system.
Figure 2 through Figure 5 depict the conceptual components of the Aquifer Pumped Hydro
system. A large array of standardized modules enables precise ramp up and ramp down
13
capability. For example, an array of 100 equally sized modules can quickly go from 1% to 100%
capacity by activating from 1 module to 100 modules in the power generation mode based on
the needs of the grid. Similarly, 100 modules in the power storage mode can decrease demand
rapidly and/or incrementally from 1% to 100% within seconds by shutting off 1 module to 100
modules. The modular pumped hydroelectric system can therefore provide both power
generation and demand response rapidly3 and in any increment desired and is more flexible
than a conventional large pumped hydroelectric project.
Figure 2: An individual unit of the APH pumped hydroelectric system
Figure 2 shows an individual unit of the APH modular pumped hydroelectric system. It consists of a reversible
pump/turbine unit at the bottom of a well shaft with a control valve 1, the well itself 2, the natural water table of the aquifer
which serves as the lower reservoir 3, the electric variable frequency motor/generator for the module 4, the remote control
and command of the valves and motor/generator of the module 5, the surface reservoir, combined inlet/outlet pipe and
flow control valve which constitutes the upper reservoir 6, and the alternating current transformers that connect the
module to the electric grid 7.
3 The term, ‘demand response’ used in the context of APH is different from the demand response potential realized by shifting the groundwater recovery operations out of peak summer hours discussed elsewhere in this report. While APH pumped storage and associated demand response capability of a multi-modular APH array can potentially occur in all hydrological year types, the latter is largely limited to dry years which is typically when groundwater is extracted for deliveries.
14
Figure 3: An APH unit in generating and storing modes
Figure 3 shows the hydraulics of the APH modular pumped hydroelectric system when generating electricity in the
generation operational mode 8. Electricity is generated when water flows down the well hole and turns the turbine 9. The
figure also shows the energy storage operational mode 10. Kinetic energy is stored as potential energy when water is
pumped up the well hole 11. Water is cycled up and down the aquifer.
15
Figure 4: Interaction of APH unit with the electrical grid
Figure 4 shows interaction of one module of the pumped hydroelectric system with the electric grid when the unit is
generating electricity 12 and how electricity flows to the grid when it needs additional power 13. It also shows the unit shut
off and on standby 14 when the grid is stable 15. Additionally, it shows the module storing energy 16 when the grid has an
oversupply of power 17. The three operational modes of the modular pumped hydroelectric system enable generation,
standby, and storing of energy providing the flexibility needed to track the demand curve of the grid precisely and rapidly.
The switch from generating electricity to storing energy nearly doubles the impact of each unit on the demand curve of the
grid. For example, a 150 kW pump/turbine has a swing of about 300 kW when it is initially pumping water with a 150 kW
motor, is turned off, and then restarts as a 150 kW generator.
16
Figure 5: APH modules within the well array
Figure 5 illustrates how all of the modules within the well array will be coordinated and controlled remotely to optimize
benefits to the grid. The array of wells 18 will cover a wide area of the grid’s distribution system. Individual modules 19 will
be controlled by a remote signal 20 that could come from a radio/microwave transmitter, the internet, or through a hard
connection. The array of wells may be located in the electric distribution system of the grid or adjacent to major electric
transmission lines. Command and control can be initiated locally or by an Independent System Operator (an entity that
manages the electricity flow and operates the electric grid to maximize the benefits to the grid).
2.1 Key Parameters for Power Generation The physical parameters that affect the power generation are “Pump-As-Turbine” (generation)
efficiency, head on turbine generator, pump flow rate, groundwater aquifer transmissivity, and
adequate land for a surface reservoir. For WSWB site, the values of these parameters are:
1. Depth to groundwater – The WSWB has a 350 ft. average depth to groundwater level which
provides the head available to drive the generation mode.
2. Pumping Capacity – The pumping capabilities of the wells are in the range of 1500 GPM to
2000 GPM, which are typical for agricultural and municipal water supply programs.
17
3. Transmissivity – The transmissivity at the site ranges from 2,900 to 3,500 feet-squared per
day (sq. ft/day) which is considered low to medium rate of water flow through the soil matrix.
Transmissivity values in the range of 5,000 to 10,000 feet-squared per day allow water to move
faster which correlates to lesser drawdown and mounding head losses and higher generation
output.
4. Surface reservoir – The facilities Master Plan for WSWB includes a reservoir that would be
used to regulate flows from the groundwater extraction well field to a high-lift pump station
used for pumping water back to the California Aqueduct. For APH analysis, it is assumed that
the well spacing will allow all wells to be served by this common reservoir. Therefore, the costs
for a surface reservoir and associated land costs have not been included in the total capital cost
of an APH unit at WSWB (Table 8).
Appendix A describes a sensitivity analysis which compares the effects of various input
parameters on the mounding head loss and power generation equations. The results show that
flow rate, transmissivity and well radius have the greatest impact on mounding losses.
2.2 Round Trip-Efficiency and Head Loss Effects The capability to generate electric power is greatly affected by the system’s component and
cumulative efficiencies. The “Round-Trip Efficiency” refers to the efficiency of the complete
operating cycle from storage (pumping) through generation (injection). As indicated in the
project proposal, the primary downside of Aquifer Pumped Hydro (APH) is its low round-trip
efficiency of around 40%-45%. Therefore, a round-trip efficiency much lower than 40% will
render an APH project non-viable (Antelope Valley Water Storage (AVWS), 2015).
The head loss component has a significant effect on the round-trip efficiency. Head loss comes
from the energy needed to pull water out of the aquifer and to push the water into the aquifer.
These losses take the form of a cone of depression (drawdown) due to pumping and a mound
that is created when water is injected into the aquifer, and are determined by site-specific
parameters which can be used to assess system efficiency. Drawdown and mounding head loss
can be measured from ground water levels during a well pumping and injection testing
program.
2.2.1 WSWB Site - Aquifer Pumped Hydro Round-Trip Efficiency
Actual well drawdown data obtained during well development was used to calculate head loss
due to drawdown. A theoretical equation was used to calculate the potential mounding.
Separate drawdown and mounding efficiencies were calculated and used to calculate the overall
round-trip efficiency of APH at WSWB site.
Table 1 provides well drawdown levels for three wells AV-2, AV-3 and AV-5 at the WSWB site.
The average of the well drawdown for the three wells after 4 hours of pumping was used to
determine head loss due to drawdown. Figure 6, Figure 7, and Figure 8 graphically indicate the
relationship between pumping time, flow rate, and drawdown.
18
Table 1: Summary of Pump Test Data for WSWB Wells AV-2, AV-3 and AV-5
Source: (Koreny, 2016)
Figure 6: Pump Test Data for WSWB Well AV-2
Source: (Koreny, 2016)
Well ID, Pumping Rate During Aquifer Test
Ground Water Level Decrease During Pumping Test
Well Drawdown (ft.) After 1 Hour
of Pumping
Well Drawdown (ft.) After 2 Hours
of Pumping
Well Drawdown (ft.) After 3 Hours
of Pumping
Well Drawdown (ft.) After 4 Hours
of Pumping
AV-2, 1400 gpm
115 120 125 133
AV-5, 2100 gpm
120 131 135 136
AV-3, 1300 gpm
101 124 140 158
19
Figure 7: Pump Test Data for WSWB Well AV-5
Source: (Koreny, 2016)
Figure 8: Pump Test Data for WSWB Well AV-3
Source: (HDR Engineering, Inc., 2016)
20
2.2.2 Head Loss Due to Drawdown and Mounding
HDR Engineering evaluated the drawdown and approximate increase in ground water levels
(mounding) that will occur if the WSWB wells were operated as injection wells (Koreny, 2016).
According to this evaluation, “The groundwater level increase in the production wells will be
approximately the inverse of the ground water level decrease during pumping. For example, if
the ground water level in the well decreases by 100 feet after pumping at 1,000 GPM, the
ground water level in the well will rise by approximately 100 feet during injection at 1,000 GPM.
This is only a rough approximation and the initial increase in ground water level mounding may
vary depending on well screen intervals, aquifer lithology in the vadose zone and other factors.”
Instead of assuming the mounding effects are the inverse of drawdown effects, this study uses
the Cooper-Jacob approximation to the Theis equation to calculate the head loss due to
mounding.
2.2.2.1 Drawdown Efficiency
Actual well development data is used to determine drawdown effects. The potential head loss
due to drawdown can then be calculated as an efficiency component as follows:
Assumptions:
Average depth to water level: 350 ft.
Reservoir Water Level: 5 ft.
Total System Static Head: 355 ft.
Drawdown (Average): 142 ft.
Total Pumping Head Required: 497 ft. (For Pumping, excludes pipe friction losses)
Efficiency Calculation:
The pump will be required to lift the water an added 142 ft.; in other words, 40% (142/355)
more pump head in addition to the system static head of 355 ft. is required to lift water into
the reservoir for a total of 497 ft. of pumping head. Therefore, the pumping stage efficiency is
less than 100% and can be calculated as follows:
Efficiency during pumping stage:
System static head = 355 ft. equates to 100% efficiency
Pumping stage efficiency = (355 ft. – 142 ft. = 213 ft.) / 355 ft. = 0.60 = 60% (average)
The following table summarizes the average efficiency for the three wells and supports the
average calculation of 60%.
21
Table 2: Summary of Drawdown Efficiency
Well No.
Drawdown (ft.) Head Required (ft.) Efficiency%
Transmissivity (sq. ft/day)
AV-2 133 222 62% 2,900
AV-3 158 197 55% 1,100
AV-5 136 219 62% 3,500
Required Head corresponds to Pumping Stage Efficiency.
2.2.2.2. Mounding Efficiency
The head loss due to mounding effects is calculated using a theoretical equation, the Cooper-
Jacob approximation to the Theis equation. This equation can be used for unconfined aquifers,
and provides the height of the injection mound. The equation was used to calculate hm =
potential mounding (feet) in the aquifer due to injection of flow through the well into the
aquifer. The equation in imperial units is:
h2.3 Q
4 3.14 TLog
2.25 ∗ T ∗ tr S
Where: Q=267.38 (injection flow rate in ft3 /minute)
S = 0.05 (Storage Coefficient)
T= 2.45 (Transmissivity of aquifer in ft2 /minute)
t = 360 (time in minutes)
r = 1.0 (well radius in (ft.))
hm = 91.7 ft. (potential mounding)
Efficiency Calculation:
System static head = 355 ft. equates to 100% efficiency
Available head during the generation stage after mounding loss = 355 ft. - 91.7 ft. = 263.3 ft.
Mounding Efficiency during generation stage = 263.3 ft. / 355.0 ft. = 0.74 or 74%
2.2.2.3 Round-Trip Efficiency Calculation
The round-trip efficiency of the system using components can be evaluated as shown in Table 3
22
Table 3: Target Average Efficiency of Aquifer Pumped Hydro Energy Storage
Component Pump/Motor System, %
Turbine/Generator System, %
1. Variable Frequency Pump Drive* 95 - 2. Power wires* 98 - 3. Motor/generator* 96 964. Pump/turbine** 80 805. Pipe friction* 98 986. Rectifier/inverter* - 937. Drawdown (213 ft. required head/ 355 ft. total head) *** 60
8. Mounding (263.3 ft. available head/ 355 ft. total head)***
74
TOTAL 42.0% 51.8%ROUND-TRIP (21.8% makes APH infeasible) 21.8% < 42%
* Target efficiencies
Sources:
**From calculations by Hydro resources (Hydro resources, 2013)
***Calculated above
2.2.3 Key Finding
The evaluation in Table 3 indicates that the round-trip average system efficiency for the site is
21.8%. This is less than the 42% estimated in the initial proposal (Antelope Valley Water Storage
(AVWS), 2015) and is too low to be practical. This low round trip efficiency for APH is much
lower than efficiency for alternative energy storage technology (% Efficiency column, Table 4).
Table 4: Energy Storage Efficiency and Costs
Technology Option Maturity Capacity Power Duration
% Efficiency
Total Cost Cost
(MWh) (MW) (hours) (total
cycles) ($/kW) ($/kW-h)
Bulk Energy Storage to Support System and Renewables Integration
Pumped Hydro Mature
1680-5300
280-530 6-10 80-82
2500-4300 420-430
5400-14,000
900-1400 6-10 (>13,000)
1500-2700 20-270
Conventional Turbine-CAES (underground) Demo
1440-3600 180 8
(>13,000)
960 120
20 1150 60Compressed Air Energy Storage (CAES):underground Commercial
1080 135 8
(>13,000)
1000 125
2700 20 1250 60
23
Technology Option Maturity Capacity Power Duration
% Efficiency
Total Cost Cost
(MWh) (MW) (hours) (total
cycles) ($/kW) ($/kW-h)Sodium-Sulfur Commercial 300 50 6 75 (4500)
3100-3300 520-550
Advanced Lead-Acid
Commercial 200 50 485-90
(2200)1700-1900 425-475
Commercial 250 20-50 585-90
(4500)4600-4900 920-980
Demo 400 100 485-90
(4500) 2700 675Vanadium Redox Demo 250 50 5
65-75 (>10,000)
3100-3700 620-740
Zn/Br Redox Demo 250 50 560
(>10,000)1450-1750 290-350
Fe/Cr Redox R&D 250 50 575
(>10,000)1800-1900 360-380
Zn/air Redox R&D 250 50 575
(>10,000)1440-1700 290-340
Energy Storage for ISO Fast Frequency Regulation and Renewables Integration
Flywheel Demo 5 20 0.2585-87
(>100,000)1950-2200
7800-8800
Li-ion Demo 0.25-25 1-100 0.25-187-92
(>100,000)1085-1550
4340-6200
Advanced Lead-Acid Demo 0.25-50 1-100 0.25-1
75-90 (>100,000) 950-1590
2770-3800
Energy Storage for Utility T&D Grid Support Applications CAES (aboveground) Demo 250 50 5 (>10,000)
1850-2150 390-430
Advanced Lead-Acid Demo 3.2-48 1-12 3.2-4
75-90 (4500)
2000-4600
625-1150
Sodium-Sulfur Commercial 7.2 1 7.2 75 (4500)
3200-4000 445-555
Zn/Br Flow Demo 5-50 1-10 560-65
(>10,000)1670-2015
340-1350
Vanadium Redox Demo 4-40 1-10 4
65-70 (>10,000)
3000-3310 750-830
Fe/Cr Flow R&D 4 1 475
(>10,000)1200-1600 300-400
Zn/air R&D 5.4 1 5.4 75 (4500)1750-1900 325-350
Li-ion Demo 4-24 1-10 2-490-94
(4500)1800-4100
900-1700
Source: (Electric Power Research Institute (EPRI) and Energy and Environmental Economics, Inc. , 2010)
This finding is further demonstrated in Table 5 below, which determines the power required for
pumping versus the power generation potential for one “Pump As Turbine” setup at WSWB. A
single setup will require 278 kW to pump groundwater into the surface reservoir and will have
a power generation potential of 62 kW. Therefore, system efficiency is 22% as predicated in
Table 3. Even if on-peak electric rates for generation are 4.5 times the off-peak rates for
24
pumping, APH will not pay for itself. Given the low average system efficiency of 22% APH is not
economically feasible for WSWB site.
Table 5: Power Calculation for One “Pump As Turbine” Setup at WSWB
Pumping Mode
Generating Mode
Components Pump/Motor System, %
Turbine/Generator System,
%1. Variable Frequency Pump Drive* 95 -
2. Power wires* 98 -
3. Motor/generator* 96 96
4. Pump/turbine** 80 80
5. Pipe friction (calculated and shown below)
6. Rectifier/inverter* - 93
Well Data: well diameter = 2.0 ft. Flow Rate: Q= 2,000 GPM = 4.45 ft./sec;
Power Requirement:
Reservoir water elevation above ground surface (ft.) 5.0 5.0
Depth to groundwater from surface (ft.) 350.0 350.0
Gross Head (ft.) 355.0 355.0
Pipe Friction loss (ft.) 33.2 33.2
Drawdown due to pumping (ft.) (field test) 142.0 -
Head loss due to mounding (ft.) (calculated) - 91.7
Net Head (ft.) 530.2 230.2
Power required for Pump Mode (kW) 278
Power potential for Generation Mode (kW) 62
* Target efficiencies
Source:
**From calculations by Hydro resources (Hydro resources, 2013)
The study scope included execution of field testing at WSWB to assess the aquifer response to a
full cycle of well pumping and well injection. Because of the low round-trip efficiency
discussed above it was concluded that conducting this test at WSWB will be premature and the
test should be postponed to a future pilot-study to determine commercial viability of the APH
technology. To that end, this section focuses on providing supporting documentation for
development of a template to evaluate APH potential at other groundwater banks including at
existing Aquifer Storage and Recovery (ASR) and recycled water projects and to identify
potential pilot sites for APH. ASR projects and recycled water projects that inject water into the
groundwater aquifer can use the injection process to generate peak hydropower without
pumping groundwater to a surface reservoir first. For these projects the energy cost for the
injection cycle (or the generation stage of APH) is a part of existing operational costs. Also,
these projects already have most of the capital infrastructure needed to generate hydropower
25
using injection wells with the exception of the electrical/mechanical package needed to
generate power and integrate the system with the electric grid.
2.3 Power Generation for a Single APH Turbine Setup Power generation for a single Aquifer Pumped Hydro unit consists of one “Pump As Turbine”
well setup, one reservoir and connection piping.
The AV-5 groundwater well at WSWB was selected for this evaluation and the potential power
generation was calculated based on the input parameters given in Table 6.
Table 6: Potential Power Generation for Well AV-5 at WSWB
Well Data:
Well Diameter ( ft.) 2.0 Injection Flow (cfs) 4.45 Pump as Turbine Efficiency
0.80
Generator Efficiency 0.96
Rectifier/inverter Efficiency
0.93
Water Density (lb./ft.3) 62.35 Power Calculations:
Transmissivity (ft.2/day) 3,526.0 5,000.0 10,000.0
Gross Head (ft.) 355.0 355.0 355.0Pipe Friction loss (ft.) 33.2 33.2 33.2
Mounding Head Loss (ft.) 91.7 70.2 37.3Net Head (ft.) 230.2 251.7 284.6
Power Generation (kW) 62.0 67.0 76.0
The Transmissivity at the AV-5 well site is 3,500 sq. ft/day. Based on a Net Head of 230.2 ft.
available to generate power, the power potential is 62.0 kW or 0.06 MW. In comparison, for
Transmissivity values of 5,000 sq. ft/day and 10,000 sq. ft/day the power generation potential
is 67.0 kW (or .07 MW), and 76.0 kW (or 0.08 MW) respectively. A 42 % increase in
Transmissivity results in a power potential increase of 8%; and a 184% increase in
Transmissivity results in a 23 % increase in power generation potential.
In order to achieve 5 MW of power generation at the WSWB site 84 wells would be required (5.0
MW/ .06 MW per well = 84 wells). The planned 62 wells at WSWB would have potential to
produce on the order of 3.7 MW. Even if Aquifer Pumped Hydro is used as an energy
generation system (rather than as a storage system) at the WSWB site, this level of power
generation would not justify the added capital expense required to deliver power to the SCE
grid.
2.4 Cost Estimates The incremental cost of installing one Aquifer Pumped Hydro (APH) storage unit includes the
following items:
Cost of 2 AF upper reservoir, including 0.5 acres of land
26
One 300 HP, 480 Vac (Volts, alternating current), 2000 GPM well
Electrical Package to generate power with the well motor, and system controller and
electrical equipment to connect the generator to the SCE grid.
Table 7 summarizes the additional capital cost of $1.6 M needed to install one APH unit at a
groundwater bank. All other capital costs such as for pipelines are assumed to be part of the
original water bank or ASR project.
Table 7: Capital Cost of Facilities for One Aquifer Pumped Hydro Unit
Aquifer Pumped Hydro Component
Calculation Cost,
$ M*
1. Surface reservoir @ 2.0 AF storage & 0.5 acres of land for 5- peak hour generation period
The 2016 master plan for WSWB facilities (GEI Consultants, Inc., 2016) includes a cost estimate of $1.32 M for a 48 AF lined reservoir, excluding engineering and contingency. For a 2 AF reservoir the cost will be = (2/48) ($1.32 M) (1.24 for engineering & contingency.) = $0.07 M. Land cost for 0.5 acres is about $0.002 M @ $3,000/acre in Kern County.
$0.072 M
2. One 300 HP well with Variable Frequency Drive (VFD)
($860,000 per well+ $130,000 per VFD) (1.24) = $1.23 M $1.23 M
3. Electrical / Mechanical Package
Motor Generator Power Electronic Controller ----------------------- $ 6,000
Grid tie inverter/rectifier--------------------------------------------------- $92,000
System Controller ------------------------------------------------------------$80,000
Electric system modifications ---------------------------------------------$20,000
Well shaft modification and pressure control equipment --------- $40,000
Electric/Mechanical Package Total $238,000 = $0.24M x 1.24 = $0.30 M
$0.30 M**
4. Total Total additional cost due to one “Pump As Turbine” Aquifer Pumped Hydro storage unit
$1.6 M
Sources:
* Unit cost estimates based on 2016 GEI master plan update for WSWB (GEI Consultants, Inc., 2016) and adjusted to include 24% more for contingencies, design, and construction management.
** Item costs estimated by author(s) based on industry research.
At WSWB, the additional capital cost needed to install one APH unit is $0.30 M due to the cost
for the addition of the Electrical and Mechanical Package as indicated in Table 8. Only the
electrical/mechanical package cost is included because the other components are assumed to
be part of the WSWB project. Assuming WSWB may be operated as an ASR project for purposes
of generating peak hydropower, the energy costs associated with pumping groundwater for
storage can be eliminated. Since any other annual operational and maintenance costs are
covered by the WSWB operating budget, no additional operating costs are included. For 62
wells, the incremental cost would be $18.6M to implement 3.7 MW of peak hour hydropower
generation or $5,100/kW.
27
Table 8: Costs to generate hydropower using existing wells at WSWB
Item Assumptions Comments
1. Well capacity 4.5 cfs each (8.9 AF/day, 2.9 mgd or 2000 gpm)
Existing irrigation wells
2. Well motor size
300 horsepower (hp) (225 kW) Typical municipal motor size
3. Depth to water Up to 350’ (depth to water)
4. Surface storage
Storage Vol. = (GPM x 5 hr. x 60 min. per hr. x 0.13368) = Storage Vol. (ft.3)
(Storage Vol. x 1.20) = Acres Required
(5 ft. x 43,560 ft.2)
For 2000 GPM, storage vol. = 80,208 ft.3 = 1.8 acre-ft. (use 2 acre-ft.)
Acres required = 0.44 acres (use 0.5 acres)
Lined, covered reservoir
5. Capital Cost to add one Aquifer Pumped Hydro Unit
From Table 6 = $0.30 M Electrical package .
6. APH Capacity 0.06 MW/well x 62 wells = 3.7 MW
7. Capital cost ($0.30 M/well)(62) = $18.6 M
8. Unit capital cost
$18.6M/3.7 MW = $5,100/kW
9. Annual O&M Zero cost assumed operating cost is covered by water bank or ASR operations.
10. Total Cost (Capital and O&M)
$18.6 M /3.7 MW = $5,100/kW
These costs are feasibility study level. More precise cost estimates should be developed as part
of a next step pilot program.
2.5 State Water Resources Control Board (SWRCB) Regulations This study also looked at the field testing requirements for the Aquifer Pumped Hydro (APH)
technology. This information informed the development of criteria for evaluating the potential
of APH technology at other groundwater banks in California.
28
All short term field testing and long term projects must comply with SWRCB and applicable
United States Environmental Protection Agency (U.S. EPA) requirements. Short term field testing
projects are for the purpose of conducting a pilot test of the technology for a specific site
where water is withdrawn from a groundwater producing well and retained at the surface for a
short period before being injected back into the groundwater aquifer. Long term projects
refer to projects that have been shown to have economic benefit and the project owner seeks to
install a permanent project.
The project team consulted Regional Water Quality Control Board (RWQCB) staff to determine
the potential regulatory requirements for both short term and long term projects.
2.5.1 Short Term Pilot Test
The regulatory requirements for short term pilot testing of APH technology are:
RWQCB permit will be required for 1 to 2-day pumping into a lined pond and 18-20 hours
discharge back into a well.
The permitting process will include formal consultation with RWQCB and submittal of a
formal permit application along with technical report and project documents.
It is expected that no treatment will be required if it can be shown that water quality will
not be affected during period of discharge.
For source groundwater that includes constituents such as Hexavalent Chromium (Cr(VI)) or
other constituents that may affect groundwater quality and may be an issue, RWQCB
will require time for additional review before determining how to proceed.
CEQA categorical exemption may be required.
2.5.2 Long Term Projects
The regulatory requirements for long term pilot testing of APH technology are:
RWQCB permit is required and the permitting process is anticipated to be more extensive
than the one described above for a pilot test.
Covered ponds are required due to algae growth, solids and bacteria issues.
Open ponds are allowed if water is treated (undergoes filtration and disinfection) before
injection (treatment requirements may vary on a case by case basis).
Monitoring wells are required for groundwater monitoring program to track impacts.
Appropriate CEQA documents would be required in all cases.
Compliance with these preliminary regulatory requirements will require additional time and
funding and should be considered in planning feasibility studies for APH4 projects.
2.6 Demand Response Potential of the Well Field 62 production wells are planned for WSWB. Each production well is expected to have a 300
horsepower (0.225 MW) motor. As determined above in Sections 2.2 and 2.3, utilizing the WSWB
4 Aquifer Storage and Recovery (ASR) projects are regulated separately by the State Water Resources Control Board Water Quality Order 2012-0010 – General Water Discharge Requirements for Aquifer Storage & Recovery Projects that Inject Drinking Water into Groundwater.
29
62 planned extraction wells in an energy generation or pumped storage system to generate
peak electric power is impractical. However, the 62 wells represent a combined demand
reduction potential of 14.0 MW. If used in a demand response program the wells could
potentially reduce the power demand on the electric grid by 14 MW. This demand response
potential is significant and can be realized by shutting down the well pumps for 5 hours a day
during weekdays in the summer months. This would result in a 4% reduction in groundwater
pumping which can be made up with a small number of additional wells. 62 wells are needed at buildout and 2 more wells are required to enable demand response (4% of 62 wells ≈ 2 wells) at
a cost of $1.07 M/well (Table 14). The surface reservoir (which is part of WSWB facilities master
plan) will buffer any impact on WSWB operations and will enable a constant flow to the WSWB
pump station.
Operating the well field in a demand response program will require a specified response time
for wells to be turned-on and turned-off following an order from California Independent System
Operator (California ISO) or an investor-owned electric utility operator. Therefore, a field test
was conducted to determine the startup and shutdown durations for manual operation of the
well field at Willow Springs Water Bank(WSWB) site. Confirming the time required for each
cycle will support decision making on whether to implement an automated cloud-based
Supervisory Control and Data Acquisition system to monitor and control the well field
equipment.
2.6.1 Automated Remote Control of the Well Field System
A key factor for implementation of demand response at WSWB is being able to shut off 62 wells
and turn them on again rapidly. The results of the field test provided on page 2 of Appendix B
show that the time required to start up each well and drive to the next well is on average 5.1
minutes; or a total start-up period of 5.3 hours with one operator. The time required to
shutdown each well and drive to the next well is similarly on average 5.0 minutes; or a total
shutdown period of 5.2 hours with one operator. It would take over 5 hours for one operator
to start-up or shutdown all 62 wells . This is not practical for operation of a large well field let
alone for a 5-hour window for demand response.
Remote activation is necessary. The legacy systems in use to remotely monitor and control well
field equipment are referred to as Supervisory Control and Data Acquisition (SCADA) systems
and include a computer server and control center located at the agency’s operations
headquarters. These systems collect data from the onsite well. The well is equipped with a
Program Logic Control data logger that sends data to the SCADA control center and the data is
stored in the control center server. With this type of system, the process of shutting down a
well is immediate and an entire well field can be programmed to start-up or shut-down on a
given schedule or at a moment’s notice.
A cloud-based Supervisory Control and Data Acquisition system such as the XiO cloud-based
Field Installed Well Control Unit replaces the typical Program Logic Control based data logger
and is widely used throughout the water supply industry to monitor and control wells. Using a
cloud-based SCADA system eliminates the need for an agency based computer server.
30
The Field Installed Unit sends all monitoring data by internet connection via an onsite modem
to the cloud. The cloud data is sent to a highly secure commercial data manager contracted
with XiO. Any authorized agency employee can access the cloud data and turn on and shut off
the well pumps from a desktop computer, laptop or smart phone. This eliminates the need and
cost for onsite server hardware and software, programming the Program Logic Control to
communicate with the server, and costly employee training to operate the system.
The team obtained a budgetary quote from XiO to install one XiO Field Installed Well Control
Unit at a single well. The cost per well ranges from $7,700 for a controller without water level
sensor to $9,700 for a controller with water level sensor and $74 per month for cloud access
and internet access (Table 9).
Table 9: Cost to Install one XiO Field Installed Well Control Unit
Controller & Options without Sensor
Unit Price Monthly Fee
Field Control Unit without water level sensor
$4,600 $39/controller (cloud services)
System Pressure monitoring $700 n/aRemote VFD $545 n/aPtP- Link IP radio with Yagi Antenna $1,100 n/aCloud-Link Cellular Modem Package $750 $35/modem (internet access)Totals $7,700 $74/monthController & Options with Sensor Unit Price Monthly Fee
Field Control Unit with water level sensor
$6,642 $39/controller (cloud services)
System Pressure monitoring $700 n/aRemote VFD $545 n/aPtP- Link IP radio with Yagi Antenna $1,100 n/aCloud-Link Cellular Modem Package $750 $35/modem (internet access)Totals $9,700 $74/month
Sources: (XiO, Inc., 2017)
The process of turning all 62 wells off and then on should be straightforward if the well field
design incorporates an automated remote on/off switch. All wells will need a slow start
capability to comply with current Southern California Edison (SCE) requirements.
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CHAPTER 3: Peak Hour Pumped Storage at Willow Springs Water Bank
Willow Springs Water Bank (WSWB) plans to use Peak Hour Pumped Storage (PHPS) to produce
hydropower during the peak hours of the day. PHPS will use pipe, pump, and reservoir facilities
that are part of the water bank. Dual use of these facilities for hydropower as well as water
storage reduces capital costs.
Power generation via PHPS can potentially occur independent of whether the water bank is
recharging, idle, or extracting water. It is expected that WSWB will recharge water during wet
years. Wet years occur about 1 in every 3 years (“wet” years as defined by California
Department of Water Resources (DWR) have occurred 32% of the time based on historical
record). Generating peak power every year is more valuable that generating it once every 3
years. Water used to generate electricity will be replaced during the non-peak hours.
Key Assumptions for PHPS analysis are summarized below:
Evening Ramp Up – Electric peak hour rates will apply during summer weekdays from about
4:00 p.m. to 9:00 p.m. for SCE and SDG&E. This is the evening ramp up of demand when
solar arrays stop generating power but the evening demand is still high. While peak
rates for the future are not known, it can be assumed that they will be high enough to
discourage pumping during the evening ramp up (California Public Utilities Commission
(CPUC), 2015).
Summer Peaks – Peak hour rates occur during the 3 summer months, 5 days a week, and for
only about 5 hours per day. This is 4% of the time. If additional power can be generated
during peak hours, a significant grid benefit can be realized. Similarly, pumping from
wells to the surface could be eliminated during peak hours as well to reduce peak
demand.
WSWB Intermittent Recharge – WSWB will recharge water intermittently (about once every
three years on average). If hydropower generation is limited to only the recharge years, a
significant opportunity is lost.
WSWB Buildout – WSWB will be built out in phases. The first phase has a recharge capacity
of 385 cubic feet per second (cfs) and an extraction capacity of 140 cfs. The second
phase has a recharge capacity of 385 cfs and an extraction capacity of 310 cfs.
Flow to and from California Aqueduct – Prior studies for WSWB assumed that water flow
from or to the California Aqueduct could vary during a 24-hour day. Since DWR will not
allow daily flow changes into the California Aqueduct, an upper reservoir is needed to
enable shutdown of booster pumping during the 5 peak summer hours.
32
3.1 Operating Scenarios Pumped storage implementation must not interfere with normal operations of the water bank.
Consequently, three operating scenarios were assessed for PHPS analysis: a recharge (wet) year,
a neutral or idle year, and an extraction (dry) year5. These scenarios are shown graphically in
Figure 9 and described in the subsequent paragraphs.
Figure 9: WSWB Hydropower Generation Operations
5 Based on Sacramento River data since 1906, California Department of Water Resources (DWR) classifies a water year (Oct 1 – Sep 30) as a wet year, an above normal year, a below normal year, a dry year or a critical year (DWR, 2017). In this report, the term “wet” indicates a wet year as defined by DWR, “neutral” is used for above normal and below normal year types, and “dry” represents the DWR defined dry and critical hydrologic year types.
33
Recharge Year (wet): A recharge year involves up to 385 cubic feet per second (cfs) of
recharge. It will occur during wet or normal year conditions. That enables a total
recharge of 280,000 acre-feet per year. 250 cfs will be used to generate electricity 24
hours a day and 185 cfs will bypass the turbine. The estimated occurrence rate is 1 year
in 3 based on historical record (32%).
Idle Year: An idle year does not have any predetermined recharge or extraction activity. 250
cfs of water will be used to generate electricity for the 5 hours daily from the upper
reservoir. The water will be replaced over the other 19 hours. It will be pumped at a flow
rate of 66 cfs to minimize pipe friction losses. 103 acre-feet of storage volume is needed
to provide 5 hours of power generation. The estimated occurrence rate is 1 year in 3
based on the historical record (33%).
Extraction Year (dry): Extractions of water from the water bank will occur in a dry year. 250
cfs will be pumped back to the California Aqueduct and 60 cfs will be delivered to the
Antelope Valley-East Kern Water Agency potable system for exchange or to the
Aqueduct. The total extraction requirement is 310 cfs. During the peak hours, electricity
will be generated by sending 250 cfs from the upper reservoir down to the generator.
103 acre-feet of storage volume is needed to provide 5 hours of generation. The 4%
extraction reduction will be made up by slightly increased extractions in the non-
summer months. The estimated occurrence rate is 1 year in 3 based on historical record
(35%).
3.2 Components and Factors for Peak Hour Pumped Storage As described in the WSWB Fact Sheet (Attachment I), the onsite facilities at WSWB include an
84” diameter recharge pipe, percolation ponds, a pump station, and 62 wells. When fully built
out, WSWB will have most of the elements needed for a pumped storage project: topography
that enables a large change in elevation, a big conveyance pipe, a pump station/turbine, and
potential sites for large upstream and downstream reservoirs. Along with operational
considerations described in the preceding section, factors such as friction losses associated
with cycling water, turbine type and costs, and availability of potential reservoir sites also affect
the ability to add pumped storage to an existing groundwater storage project.
3.2.1 Reservoir Site Analysis
A pumped storage project needs both an upper and a lower reservoir. This enables hydropower
operations regardless of whether the water bank is recharging, extracting, or is idle. Water is
pumped to the upper reservoir during the off-peak period. It is drained down to the lower
reservoir during the on-peak period. Power is generated when water flows through the turbine
generator and into the lower reservoir. This can occur 365 days a year.
Originally, it was assumed that DWR may allow the California Aqueduct to serve as the upper
reservoir by enabling daily flow variation. Subsequent discussions with DWR staff indicated
that the department is adamantly opposed to this (Craig Trombly, personal communication,
August 5, 2016). Consequently, potential sites for the upper reservoir were identified near the
34
California Aqueduct. All sites meet the criteria of target reservoir water surface elevation of
approximately 2950’. Figure 10 shows a map of the potential upper and lower reservoir sites.
Figure 10: Potential Upper and Lower Reservoir Sites
The upper and lower reservoirs isolate the operations of the Aqueduct from the hydropower
operations. They also isolate WSWB operations from hydropower operations. This ensures that
power generation will not interfere with the operation of other water banking infrastructure.
3.2.1.1 Potential Upper Reservoir Sites
35
Four possible sites with enough land at the right elevation for the upper reservoir were
identified (Table 10). Two are north of the Aqueduct and two are south of it. Potential sites
were identified based on whether the land is vacant, whether it is at the right elevation, whether
14 acres or more of land is available, and proximity of the site to the WSWB turnout structure.
Available parcels range from 13 acres to 114 acres as shown in Appendix C-1. Phasing can be
accomplished by utilizing more than one site or one of the larger parcels.
The two reservoir sites north of the Aqueduct are at elevations lower than the 2955’ water
surface in the Aqueduct. These sites are 5’ to 25’ lower than the Aqueduct’s water surface. To
make these sites viable, a 250 cfs, 378 HP low lift pump station (10’ to 30’ lift) and piping to CA
Aqueduct will be needed to pump the water back into the Aqueduct. Most years, WSWB will be
idle or recharging water. Pumping is only needed during dry years.
Table 10: Summary of Potential Land for Upper Reservoir
Location Assessor Identification Number (AIN)
Elevation Size, Acres
Value/acre based on
taxes
Land Use
North of Aqueduct 3236-020-003 2930’ 17 $2,813/ac. Vacant North of Aqueduct 3236-020-004 2950’ 13 $3,028/ac. Vacant South of Aqueduct 3236-021-009 3000’ 114 $1,044/ac. Vacant South of Aqueduct 3236-020-008 3000’ 15 $3,333/ac. Vacant
Sources:
APN, Land Use, Value and Size (Los Angeles County Office of the Assessor, n.d.)
Elevation (Google Earth)
The two reservoir sites south of the Aqueduct are at elevations higher than the 2955’ water
surface in the Aqueduct. They are 45’ higher than the Aqueduct’s water surface. An upper
reservoir located at any of these two sites will require a lift of 50’ to receive water from the
Aqueduct. Appendix C-2 through Appendix C-5 show Google Earth images of all of these four
sites.
One upper reservoir site that has been considered is the Los Angeles Department of Water and
Power’s (LADWP’s) abandoned Fairmont Reservoir #1. This site is at an elevation of 3033’ and
provides the highest lift differential of the reservoir sites considered. It is also vacant. WSWB
has not yet approached LADWP about using this location due to the availability of other
alternative sites.
3.2.1.2 Potential Lower Reservoir Sites
Four lower reservoir sites were also considered and are shown in Appendix C-6. All of these
sites are on land owned by WSWB. This eliminates the need to purchase new right-of-way for
these sites. Table 11 describes the four lower reservoir sites of interest, along with the
corresponding elevation differences.
The lower reservoir is an integral part of the facilities needed to build out WSWB. This is
because the control of 62 wells is too difficult operationally unless the reservoir provides a
fixed water surface level. The fixed hydraulic grade line also makes variable speed drives
36
unnecessary. Finally, it serves as the well for the pump station. It does double-duty as storage
volume to enable both pumped storage and demand response by the wells.
Table 11: Summary of Potential Land for Lower Reservoir
Location Assessor Parcel
Number (APN)
Elevation Size, Acres
Cost ($) Land Use Owner
Gaskell & 160th 261-196-24 2640’ 25 0 Vacant WSWB
Willow and 150th 359-041-11 2630’ 25 0 Vacant WSWB
Gaskell & 150th NW 359-041-12 2620’ 25 0 Vacant WSWB
Gaskell & 155th NW 359-041-13 2630’ 25 0 Vacant WSWB
Sources:
APN, Land Use, and Size (Kern County California, n.d.)
Elevation (Google Earth)
3.2.2 Selection of Generator Type
With pumped storage, it is possible to generate electricity by running the pump in reverse as a
turbine generator. This is possible with reaction pumps like Francis or Kaplan turbines (Figure
11). Running the pump in reverse is the simplest and least expensive way to generate electricity.
The use of a reaction turbine, however, may create hydraulic control problems. For example,
valves and controls are needed to make sure the pump never becomes a “runaway turbine”.
Hydraulic surge is also more difficult to deal with, especially if the pipe and pump system is
being shut off regularly. Also, dual purpose pump/turbines are generally not available in a size
smaller than 50 MW. Units available in the 5 MW size limit the options to a separate pump and
turbine system.
Figure 11: Francis Turbine
37
Source: (Eternoo Machinery Co., Ltd, n.d.)
An impulse turbine like a Pelton Wheel (Figure 12) is more expensive to install than running an
existing pump in reverse. However, an impulse turbine is more cost effective overall than a
reaction turbine because factors such as reduced hydraulic control, surge costs and the lack of
a suitable pump/turbine can be avoided.
Figure 12: 5-Jet Pelton Wheel Impulse Turbine (Elevation and Plan Views)
Source: (HDR, 2017)
38
3.2.3 Total Energy Losses
Pipe friction and pump/turbine energy efficiency losses must be added to the static head to
calculate the total dynamic head. The total dynamic head determines the power needed for the
pump station. It also determines the amount of energy that can be generated from a turbine.
Table 12 lists the pipe friction and pump and turbine efficiency loss assumptions used for this
project.
3.2.3.1 Static Lift
The static “lift” is the elevation difference between the upper reservoir and the lower reservoir.
This elevation difference determines the amount of head or lift available to generate energy.
The larger the lift, the better. The upper reservoir sites considered are located near the
California Aqueduct at W Avenue H and 170th St. W. They range from elevations of 2930’ to
3000’. The lower reservoir sites range in elevation from 2620’ to 2640’. This creates a range of
potential lifts from 290’ to 380’. A 330’ static lift is used for power and hydraulic calculations
in this report. This is based on the most likely ultimate sites for the upper and lower reservoirs.
3.2.3.2 Pipe Friction
The largest energy efficiency losses come from pipe friction. These losses are 16’, 47’, and 71’
for an 84” dimeter pipe that is 9.25 miles long and has water flowing at 140 cfs, 250 cfs, and
310 cfs, respectively. These friction loss rates are based on HDR’s hydraulic calculations for
WSWB site (HDR, 2017)
3.2.3.3 Pump and Motor Efficiency
Pump and motor efficiency affects energy losses. A pump efficiency of 87% and a motor
efficiency of 96% is used for this study. Similarly, a turbine efficiency of 91% and a generator
efficiency of 96% is used for this study. These values are based on the pumped storage
operation characteristics provided in HDR report (HDR, 2017) and were developed from
standard industry assumptions. The turbine type assumed is a multi-jet Pelton Wheel impulse
turbine because a Francis type reaction turbine is not available in the 5 MW size range.
3.3 Calculation of Hydropower Generation Table 12 summarizes the potential hydropower generation at WSWB. The potential is split into
two phases to match the planned phased buildout of WSWB. Static lift is 330’ for both phases.
Phase 1 flow is 140 cubic feet per second (cfs). Phase 2 flow is 250 cfs. The size of both the
upper and the lower reservoir for Phase 1 is 58 AF, requiring 14 acres of land. The size of both
the upper and the lower reservoir for Phase 2 is 103 AF, requiring 25 acres of land (Table 13).
This results in a capacity of 3.2 MW for the Phase 1 generator and 5.2 MW for Phase 2 generator
(Table 12).
The size of the pump/turbine is determined by power (horsepower (hp)) needed for the pump
station The detailed hydropower estimates are shown in the HDR report (HDR, 2017).
Table 12: Reservoir, Generator, and Pump Power Calculations
39
Phase Flow, cfs
Generator/Turbine or Pump/Motor
Efficiency
Static lift
Pipe Friction
Loss
Total Dynamic
Head
Turbine or Pump Power
Phase 1 Generator
140 96% & 91% 330’ 16’ 314’
3.2 MW
Phase 1 Pump
140 87% & 96% 330’ 16’ 346’
4.9 MW(6,600 hp)
Phase 2 Generator
250 96% & 91% 330’ 47’ 283’
5.2 MW
Phase 2 Pump
310 87% & 96% 330’ 71’ 401’
10.2 MW(13,700 hp)
3.4 Extended Duration Battery Potential Pumped storage at WSWB has the potential to function much like an extended duration battery.
Instead of a 5-hour discharge period, if the upper and lower reservoirs are made larger, the
power generation can be extended to up to 12 hours daily if this benefits the grid. Pumped
storage could also be used to provide power during an emergency or during a potential early
morning ramp up.
The upper reservoir volume is sized to match the volume of the lower reservoir. This enables
one complete pumped storage cycle during a 24-hour period.
The potential for extending the duration of power generation is demonstrated in Table 13. For a
5-hour energy generation duration, the upper reservoir needs 25 acres of land when the WSWB
is fully built out. The lower reservoir also needs about 25 acres of land. This calculation
assumes 5’ maximum berm height plus 1’ of freeboard to avoid being considered a dam (a dam
is >6’ berm height). A lined and covered earthen bermed reservoir is assumed. It is also
assumed that the total area needed for each of the reservoirs includes 20% more land than the
wetted area to account for berms and access roads.
Table 13: Summary of Upper and Lower Reservoir Sizing
Reservoir Elevation Water Depth
Volume Surface Area
5-Hour Size*
8-Hour Size*
12-Hour Size*
24-Hour Size*
Upper, Phase 1
2950’ 5’ 58 AF 12 acres 14 acres 22 acres
33 acres 66 acres
Upper, Phase 2
2950’ 5’ 103 AF 21 acres 25 acres 40 acres
60 acres 120 acres
Lower, Phase 1
2620’ 5’ 58 AF 12 acres 14 acres 22 acres
33 acres -
Lower, Phase 2
2620’ 5’ 103 AF 21 acres 25 acres 40 acres
60 acres -
*Includes 20% more land for non-wetted area.
The 12-hour duration reservoir requires 60 acres. Longer durations like 24-hour generation are
possible, but it would be a one-time discharge because 12 hours is needed to refill the upper
reservoir daily. Phasing of the water bank requires that a second reservoir be built that is
roughly the same volume as the first reservoir to handle 250 cfs flows.
40
Longer durations of power generation for up to 12 hours may help fill the gap between
batteries and large hydropower resources. It could also be used to help address a potential
second daily spike in demand in the early morning. The ability to generate electricity for up to
12 hours could be utilized as needed to add more power to the grid. The only requirement is
that the upper and lower reservoirs are built large enough to enable extended power
generation.
3.5 Demand Response Potential of the Pumping Plant Demand response is the ability to reduce use of electricity when the grid has a shortage. This is
possible at WSWB in an extraction year. Similar to the demand response potential of the well
field described in Section 2.6, pumps at the pumping plant also have the potential to provide
demand response. Like the well pumps, the pumping plant pumps could be shut off for 5 hours
a day during years that water is being pumped back to the California Aqueduct. Extraction is
expected to occur 1 year in 3 during dry conditions. The upper reservoir will maintain a
constant flow to the Aqueduct with a small, low-lift pump (10’) at the reservoir site.
The demand response potential of the pumping plant corresponds to the size of the pumps, or
10.2 MW. It can be realized by shutting down the pumping plant to the Aqueduct for 5 hours a
day during weekdays in the summer months. The 4% reduction in summer water delivery to the
Aqueduct can be made up during deliveries at other times of the year because DWR allows 9%
peaking for its facilities.
3.6 Cost Estimates The incremental capital cost of installing Peak Hour Pumped Storage (PHPS) and demand
response includes the following items:
Cost of a 103-AF upper reservoir, including 25 acres of land
Cost of a 250-cfs, 378 hp low lift pump station and piping to CA Aqueduct
Cost of two new 3.4-MW impulse turbine
The cost of 4% additional well capacity to enable demand response (2 wells)
All other costs for pump stations, pipelines, lower reservoir, and wells are part of the original
water bank and do not increase project costs. Table 14 summarizes the cost of the additional
capital cost needed to install PHPS and incorporate demand response at WSWB. The total cost
estimate is $10.0 M to implement 5.2 MW of Peak Hour Pumped Storage and 24.2 MW of
demand response.
These costs are feasibility study level. More precise cost and schedule estimates will be made
during preliminary and detailed design, including whether the project should be built out in
two phases or built out completely in one step only.
There are no additional costs needed to provide 24-hour power generation in recharge (wet)
years. Hydropower generation during wet years supplements the demand response and peak
hour power generation benefits during dry years.
41
Operating costs will increase because the pump station will be operated during recharge, idle,
and extraction years. If hydropower was not part of the WSWB, the pump station would be
operated only during extraction years. The annual operating cost of the pump station is
estimated at $100,000/year based on adding one staff as an operator ($100,000/operator/year).
This has a present worth of $1.06 M6.
Table 14: Capital Cost of Facilities for PHPS and Demand Response
Component Details Cost, $ M 1. Upper reservoir @ 103 AF & 30 ac. of land*
Upper reservoir is only needed if pumped hydro is built. The 2016 master plan for WSWB facilities (GEI Consultants, Inc., 2016) includes a cost estimate of $1.32 M for a 48 AF lined reservoir, excluding engineering and contingency. For a 103 AF reservoir the cost will be = (103/48) ($1.32 M) (1.24 for engr. & contingency.) = $3.51 M. Land cost for 30 acres is about $0.09 M @ $3,000/acre in Kern County.
$3.6 M
2. 250 cfs low lift pump @ 378 hp, 10’ lift*
[378 hp ($1,000/hp) + 250 cfs ($500/cfs)] (1.24) = $0.62 M. Pumps water from upper reservoir to the Aqueduct during extraction years.
$0.6 M
3. 5.2 MW of impulse turbine capacity**
Two 3.4 MW 5-jet Pelton Wheel turbines @ $1.5 M ea. and 24% for engineering & contingencies.
$3.7 M
4. Two more 300 HP wells @ $1.07 M each*
($860,000 per well) (2) (1.24) = $2.13 M Two more wells to make up the water not pumped during the 5-hour shutdown on peak days.
$2.1 M
6. Total capital cost Total additional cost due to Peak Hour Pumped Storage and demand response
$10.0 M
Sources:
* Unit cost estimates based on 2016 GEI master plan update for WSWB (GEI Consultants, Inc., 2016) and adjusted to include 24% more for contingencies, design, and construction management.
** (HDR, 2017)
3.7 CEQA Considerations Construction of an upper reservoir will likely trigger the need to prepare and adopt either a
Subsequent Environmental Impact Report (EIR) or a Supplemental EIR tiered off the existing
WSWB adopted California Environmental Quality Act (CEQA) EIR. No action was taken as part of
this project that might trigger CEQA. Instead, design and construction of the upper reservoir
were deferred until the PHPS project has proven to be cost effective.
If PHPS is proven to be economically feasible and full-scale implementation is desired it is
anticipated that the project would need to obtain Federal Energy Regulatory Commission (FERC)
approval to generate electric power to be provided to the electric grid. It is anticipated that the
pumped storage project would qualify for a Conduit Exemption for Small/Low- Impact Hydro
projects that are planned to generate less than 40 MW of power, and must be located on a
Conduit used for agricultural, municipal, or industrial consumption. The exemption only
covers the powerhouse and pipeline connections to the Conduit. Other FERC Conduit
Exemption project provisions include:
6 The present worth factor used is 10.6 based on a discount rate of 7% and a 20-year planning period.
42
May be subject to Federal and State fish and wildlife conditions under section 30(c) of the
Federal Power Act (FPA), 16 U.S.C. § 823a(c);
3-stage consultation required under Code of Federal Regulations (CFR), 18 C.F.R. § 4.38;
however, with concurrence from all resource agencies, the applicant may seek waiver of
the consultation requirements under 18 C.F.R. § 4.38(e);
Conduit Exemption projects are categorically exempt from preparing an environmental
document such as an Environmental Assessment (EA) or Environmental Impact
Statement (EIS) under 18 C.F.R. § 380.4(a)(14) that would not be prepared by FERC
unless determined necessary.
If a Conduit Exemption is obtained from FERC, then the only environmental document required
for the pumped storage project is either a Subsequent EIR or Supplemental EIR as described in
the first paragraph above. The Subsequent EIR or Supplemental EIR would address impacts
from the upper reservoir, powerhouse, pipeline connections, and an electric transmission line
to send the generated electric power to the grid.
If the pumped storage project is unable to obtain a Conduit Exemption, then it is likely that the
FERC Traditional Review process would be implemented to obtain a License to generate electric
power. Under the licensing process a Federal nexus would exist which would trigger the need
to prepare an EIR/EIS to comply with CEQA and NEPA (National Environmental Policy Act).
3.8 Summary of WSWB Pumped Storage Analysis Potential power generation and demand response at WSWB is summarized in Table 15.
Table 15: Power Generation and Demand Response Potential at WSWB
Application Peak Hour Power (every
year)
Recharge Year Power
Recharge Year
Occurrence
Demand Response
Extraction Year
Occurrence 1. Turbine or Pump*
5.2 MW for 5 hours
5.2 MW for 24 hours
32% 10.2 MW for 5 hours
35%
2. Well field (62 wells, 300 hp each)
Impractical Impractical - 14.0 MW for 5 hours
35%
3. Totals 5.2 MW 5.2 MW 32% 24.2 MW for 5 hours
35%
* To simplify the results, only the Phase 2 power and demand response values are shown.
In a dry year WSWB will extract water and pump it to the California Aqueduct. The net peak
hour power benefit in a dry year is the value of the electricity generated (5.2 MW) plus the
reduced power for groundwater pumping (14.0 MW) plus the reduced power for the pump
station (10.2 MW). This totals 24.2 MW of combined energy benefits. Effectively, energy
benefits are leveraged by the combination of power generation and demand response. This will
occur 35% of the time. The incorporation of demand response at pumping plants is possible at
any site that has room for upper and lower reservoirs and incorporates a lift to get water into
or out of the bank. Demand response using well pumps is possible at any site that has room for
a small reservoir and wells with remote on/off switches (Figure 13).
43
In years when the bank is idle, the net peak hour benefit is the value of the 5.2 MW of electricity
generated. This will occur 33% of the time.
In wet years, WSWB will recharge water into the bank’s percolation ponds. Recharge flow is a
constant 250 cfs. This will generate electricity 24 hours a day for the entire year. The benefit is
the value of the 5.2 MW of electricity generated constantly over the year. This occurs 32% of the
time.
The hydrologic cycle is random. Consequently, the combined benefits of power generation and
demand response are unpredictable. The years in which these benefits occur are not correlated
to other load-inducing factors such as hot summer temperatures.
For implementing PHPS technology at WSWB, turbine type will need to be further evaluated to
verify that a reaction pump cannot be run in reverse as a generator in the 5 MW size range and
a separate impulse turbine is required. This will involve preliminary design. The cost
ramifications are about $3.7 M. This does not include the cost of additional hydraulic and surge
control that may be needed. The best sites and optimum sizes for the upper and lower
reservoirs will also need to be determined. Additionally, the right-of-way will need to be
acquired for the upper reservoir and the facilities plan updated to set aside land at WSWB for
the lower reservoir.
Figure 13: A Groundwater Well at Willow Springs Water Bank
Figure 13 shows one of the smaller groundwater wells (with a 200 hp motor) at Willow Springs Water Bank (WSWB). Most
groundwater banking projects have recovery wells that can potentially be automated for demand response.
Photo Credit: Tommy Ta, Antelope Valley Water Storage, LLC (AVWS)
Results of the WSWP specific evaluation were incorporated into the Peak Hour Pumped Storage
(PHPS) and Aquifer Pumped Hydro (APH) templates. The templates allow the calculation of
pumped storage, hydropower generation, and demand response potential of the well field and
44
pump station(s) for other groundwater banking projects. The permitting requirements for both
the pumped storage technologies have been briefly discussed in the context of implementing
pumped storage at WSWB. As discussed in Chapter 4, a next-step pilot project may need to
consider permitting in more detail.
45
CHAPTER 4: Statewide Applicability Analysis
This chapter describes the technical feasibility of implementing the Peak Hour Pumped Storage
(PHPS) and Aquifer Pumped Hydro (APH) technologies at groundwater banks around the State.
In determining the potential of any storage system, ease of deployment and scalability plays an
important part. Therefore, the feasibility criteria identified in the preceding chapters were used
to evaluate statewide potential of the pumped storage at groundwater banks. The two energy
storage systems are not mutually exclusive and a single groundwater banking facility can
potentially deploy both. To determine the statewide potential, the study takes into account
various kinds of groundwater banking operations including recycled water projects. Recycled
water projects that use injection wells need only have the generating cycle of APH and therefore
may have considerable potential for generating peak energy. This is because in most instances,
recycled water needs to be recharged daily. Recycled water also has most of its particles
removed so there is lower risk of well screens getting clogged.
Groundwater banking projects around the state also have capability to provide demand
response during extraction years. Estimates of the statewide demand response potential and its
value were also developed as part of this project.
An important component of the statewide analysis is development of a template that makes it
possible to evaluate pumped storage potential for any groundwater banking project including
those that are currently being planned to recharge the overdrafted groundwater basins around
the State of California.
4.1 Literature Review and Statewide Survey Given the number of groundwater banking agencies and complexity and diversity of their
individual conveyance systems and operational metrics, a statewide survey was developed to
obtain key information to determine pumped storage system feasibility at various groundwater
banking sites. Information from the survey responses was supplemented by literature research
with the goal of identifying promising sites for pumped storage and formulating follow up
questions to the surveyed agencies that pass the preliminary screening. To that end, the
literature review focused on researching the urban water management plans and other reports
and analyzing this information in conjunction with the survey responses. The results from both
of these data collection activities are summarized in Appendix D-1 through Appendix D-7.
Statewide survey outreach started in Dec 2016. All of the agencies on the List of CA
Groundwater Banking Projects (Antelope Valley Water Storage (AVWS), 2016) were contacted at
least twice. The received survey responses were incorporated into the statewide master
database compiled for this study. The response rate was found to be inadequate to provide a
statewide picture of the pumped storage potential at groundwater banks particularly with
regards to Peak Hour Pumped Storage (PHPS).
46
4.2 Analysis Approach for Peak Hour Pumped Storage To determine potential of PHPS technology, information on flow rate and elevation difference
between source conveyance and recharge basin(s) is necessary. Previous studies have
acknowledged the difficulty of obtaining comprehensive data about specific water system
facilities and operational flows since this information is generally not available in public
domain for security reasons (Navigant Consulting, June 2006).
Therefore, an alternative approach to PHPS statewide analysis was adopted. Since hydropower
generation and PHPS both require similar criteria (namely sufficient head and flow) for
successful implementation, statewide estimates for small hydropower potential can be used to
give a preliminary estimate of Peak Hour Pumped Storage (PHPS) potential at groundwater
banking projects.
An existing study, Statewide Small Hydropower Resource Assessment (Navigant Consulting, June
2006) estimates the statewide potential for small hydropower in manmade conduits (pipelines,
aqueducts, irrigation ditches, and canals) by using annual water entitlements to extrapolate the
computed small hydropower generation potential for the surveyed population to the
population of water agencies that were not surveyed. The study recognizes the potential of in-
conduit hydropower to be used in conjunction with pumped storage facilities for generating
power during peak periods.
The developable hydropower potential in man-made conduits is estimated to be 140 MW- 170
MW which is 50-60% of the statewide undeveloped small hydropower nameplate potential (278
MW) (Navigant Consulting, June 2006; Kane, 2005). The statewide in-conduit small hydropower
coincident peak capacity occurs during July and August and is estimated to be 230 MW
(Navigant Consulting, June 2006; Kane, 2005). Annual water entitlements and available county
level coincident peak hydropower capacity data was used to interpolate small hydropower
potential for the groundwater banking agencies. For example, if groundwater banking water
agencies located in a particular county have total water entitlements that constitute 39% of the
total county water entitlements, the cumulative hydropower production potential for these
districts was estimated to be 39% of the countywide hydropower potential (kW) of all (both
groundwater banking and non-groundwater banking) districts (Appendix E shows these
calculations.) In the reference statewide small hydropower study, the small hydropower
generation potential was extrapolated using estimation factors that were developed based on
size, primary water system function (irrigation vs. municipal) and geographic region (north,
central and south) of the surveyed and non-surveyed agencies. Because of unavailability of the
entire reference study database, the interpolation method described above takes into account
only the annual water entitlements and geographic region. It is acknowledged that annual water
entitlements are insufficient to compute hydropower or pumped storage potential in absence of
other information, particularly head losses. However, it can be assumed that the available static
head7 to generate power does not differ significantly for the water districts located in the same
county. This assumption is borne out by the findings of the reference study which indicate that
7 Elevation difference between the upper and lower reservoir.
47
the different regions of the state have distinct advantages or drawbacks regarding available
head and operational flows (Navigant Consulting, June 2006). Additionally, analysis of
countywide annual water entitlements data from Statewide Small Hydropower Resource
Assessment (Navigant Consulting, June 2006) in conjunction with countywide small hydropower
potential data from California Small Hydropower and Ocean Wave Energy Resources (Kane,
2005) shows that for a particular region, counties with higher annual water entitlements
generally have higher small hydropower generation potential than those with lower annual
water entitlements . Therefore, it can be assumed that the annual water entitlements are
largely responsible for the difference in hydropower potential between the water districts
situated in the same county8. This estimated countywide small hydropower potential for
groundwater banking agencies was rolled up to give the potential for each hydrologic region
(Table 16).
4.2.1 Statewide PHPS Potential at Groundwater Banking Projects
The cumulative PHPS potential of groundwater banking agencies will be lower than the
cumulative small hydropower potential (Table 16) because PHPS differs from small hydropower
in several key ways which constrain the statewide PHPS potential:
1. A minimum head of 9 feet and a minimum flow rate of 120 cfs is required to install a small
hydropower facility in an existing manmade conduit (Navigant Consulting, June 2006).
Although the small hydropower criteria flow rate of 120 cfs is a reasonable minimum threshold
for PHPS, the elevation difference between the upper reservoir and lower reservoir would need
to be much greater than 9 feet for PHPS to be economically feasible at a site. Additionally, pipe
length has a significant impact on pipe friction and pipe friction losses can be kept to a
minimum for a given flow rate at sites where the length of pipe between upper reservoir and
generator can be minimized. The uncertainty in the computed statewide PHPS potential is
therefore largely due to information gaps regarding elevation data and length of conveyances.
2. The reference study (Navigant Consulting, June 2006) assumes a “run of the river (canal in
most cases)” hydropower development with no more than part day storage. PHPS will need
closed conduits (pipelines) to cycle the water. A previous study9 (California Department of
Water Resources, April 1981) indicates that most of the pipelines with small hydroelectric
generation potential are clustered in the southern portion of the state and that in this region,
majority of the man-made conduits that have hydropower potential are pipelines. In contrast, in
northern and central regions, majority of conveyance systems with hydropower potential are
canals. Besides the large operational flows, the density of pipelines in Southern California is
another reason to focus on this region for potential PHPS opportunities or demonstration
projects. This also implies that particularly in northern and central regions of the state, PHPS is
8 This does not imply that higher flow rates or volumes will consistently result in higher hydropower potential. As described in the WSWB PHPS analysis (HDR, 2017) conducted for this project, the friction loss rate in a given pumped storage operation increases rapidly after the flow rate exceeds a certain point.
9 The map, “Potential Small Hydroelectric Sites at Existing Hydraulic Facilities” in “Bulletin 211 Small Hydroelectric Potential at Existing Hydraulic Structures in California” shows dam, canal, and pipeline facilities that have small hydroelectric potential.
48
lower than the small hydropower generation potential (Table 16). This is why the statewide
PHPS was assumed to be 50% (44 MW) of the total small hydropower generation potential of
about 88 MW.
3. The reference study identified 128 renewable portfolio standard (RPS) eligible small
hydropower sites for the water purveyors that were surveyed. Given that the in-conduit
hydropower potential on large regional conveyance systems has largely already been developed,
67% of these potential sites had capacity less than 1 MW (Navigant Consulting, June 2006).
Economic evaluation (discussed in Chapter 5) indicates that PHPS facilities with characteristics
similar to that of WSWB and with generating capacity of 5 MW will find it difficult to be
economically viable if operated as a pumped storage system during neutral years and as an
energy generator during wet years. Addition of dry year demand response can potentially make
these systems economically feasible and will also result in greater economic and grid benefits.
4. The research and survey results indicate that the pump back operations of many
groundwater banking agencies do not involve pumping to the source conveyance. Even if they
did, the use of large regional conveyance systems for PHPS is unlikely to be allowed10 which
necessitates construction of an upper reservoir even for groundwater banking agencies situated
close to a large conveyance. Many groundwater banking districts (particularly the irrigation
districts) may already have a lower reservoir but would likely need to construct an upper
reservoir to implement PHPS. Sites that are located in highly urban and dense areas with few or
no options available for reservoir siting will not be able to develop PHPS.
5. The undeveloped small hydropower potential is greatest in southern region followed by
northern and central regions (Navigant Consulting, June 2006). The distribution of regional
PHPS potential is expected to be similar. Groundwater storage capacity is not a good indicator
of the PHPS potential. Central California has significant groundwater storage capacity but low
small hydropower and pumped storage potential because of insufficient head and flow. The
water systems in Northern California have higher head and flow but relatively few groundwater
banking agencies and closed conduits with small hydroelectric potential. Therefore, PHPS
potential appears to be largely limited to Southern California which region has several large
groundwater banks (Appendix E) and higher density of pipelines. However, this potential is
curtailed because of the predominantly urban nature of the region which may make land
acquisition for an upper reservoir difficult.
Assuming generation for 5 hours 365 days a year, implementing PHPS at groundwater banks
across the State can potentially provide 80,300,000 kWh (80 gigawatt-hours) of energy annually.
The value of this generation at different locations may be different depending on the extent to
which a PHPS facility contributes to improving grid operations at a particular location. This
value analysis is beyond the scope of this study and for the purposes of benefits evaluation, a
single annual value of pumped storage was calculated and used.
10 California Department of Water Resources is opposed to the use of California Aqueduct as the upper reservoir. (Personal communication with Craig Trombly, California Department of Water Resources, August 5, 2016)
49
50
Table 16: Peak Hour Pumped Storage (PHPS) potential at Groundwater Banking Projects
Geographic Region Hydrologic
Region
Annual Water Entitlements
(AWE) for Groundwater
Banking Agencies
Estimated Small Hydropower
Potential (kW) for Groundwater
Banking Agencies
Estimated Statewide
Pumped Storage Potential (kW) for
Groundwater Banking
Agencies a
N Sacramento River
422,000
3,102
44,000
S South Lahontan b
466,800
12,050
N,C San Francisco Bay
512,500
4,952
S Colorado River
546,200
1,926
C,N San Joaquin River
609,000
4,686
S South Coast
2,129,590
30,173
N,C,S Tulare Lake
4,608,994
30,653
Total
9,295,084
87,542
a Estimated statewide pumped storage potential is assumed to be half of the statewide small hydropower potential for
groundwater banking agencies due to the constraints discussed in the section, "Statewide PHPS Potential at Groundwater
Banking Projects.”
b Includes water entitlement and Peak Hour Pumped Storage (PHPS) potential for Antelope Valley Water Storage (AVWS)'s
groundwater banking project, Willow Springs Water Bank (WSWB).
4.3 Aquifer Pumped Hydro Potential Relative to PHPS, literature review for APH was more successful in that it yielded detailed
information for several groundwater banking facilities which was used to screen agencies for
APH feasibility. Transmissivity was one of the key criteria used in the screening. The sensitivity
analysis results discussed in Appendix A-2 indicate that transmissivity is one of the primary
factors in determining the round trip losses. Aquifers with high transmissivity allow the
injected water to move away faster from the site of injection which decreases the head losses
associated with mounding. In the absence of high transmissivity, the round trip losses
significantly reduce the statewide potential for APH as described in the Willow Springs Water
Bank (WSWB) APH assessment in Chapter 2.
4.3.1 Aquifer Storage and Recovery (ASR) Projects
Aquifer Storage and Recovery (ASR) projects are a type of groundwater banking projects that
use injection wells to store water in the aquifer when water is available and later recover the
water from the same well. ASR projects are typically sited in areas where the underlying aquifer
51
has high transmissivity. Most ASR projects in Western US typically have transmissivity in the
range of 5,000 to 10,000 sq. ft/day or greater (Antelope Valley Water Storage (AVWS) LLC,
2016). Additionally, for these projects, the head losses are halved because groundwater does
not need to be first pumped to a surface reservoir. Given the above, the well field at these
projects can potentially be used to generate hydropower during recharge activities. However,
further evaluation using statewide template and results from economic analysis indicates that
the capital costs associated with retrofitting injection wells for hydropower production may be
cost prohibitive for most agencies. Whether or not energy generation is viable at a particular
ASR project will greatly depend on the project’s location and how well the generating capacity
at that specific location compares to the costs for installing the generator and electrical
package.
4.3.2 Recycled Water for Direct Injection
Recycled water projects that inject treated water into the ground as part of their routine
operations obviate the need to pump the groundwater to a surface reservoir prior to its
injection. These projects (as Aquifer Storage and Recovery (ASR) projects discussed above) have
higher potential to generate peak energy cost-effectively than comparable Aquifer Pumped
Hydro (APH) projects. As with APH projects however, the injection process can cause clogging
and other complications if the water is not pretreated using appropriate methods. This study
looked at which tertiary treatment methods (membranes, gravity filters or cloth filters) result in
a low enough turbidity to make recycled water suitable for direct injection.
The Division of Drinking Water (DDW) has treatment requirements for producing recycled water
for groundwater recharge. For both surface spreading and subsurface injection projects, the
recycled water must meet the disinfected tertiary recycled water treatment requirements of
Title 22 of California’s Water Recycling Criteria. The requirements for projects recharging water
via direct injection are stricter than those for surface spreading projects and preclude the use
of cloth filters or gravity filters. Microfiltration with reverse osmosis and disinfection is
required before recycled water can be injected (Environmental Science Associates , 2005; RMC
Water and Environment, 2007; RMC Water and Environment, 2016). The turbidity of the filtered
wastewater that has been passed through a microfiltration, ultrafiltration, nanofiltration, or
reverse osmosis membrane does not exceed 0.2 Nephelometric Turbidity Units (NTU) more than
5 percent of the time within a 24-hour period and 0.5 NTU at any time (RMC Water and
Environment, 2016; State Water Resources Control Board Division of Drinking Water, 2014).
Literature review indicates that at present there are four large scale groundwater recharge
operations in California that inject recycled water into the ground. All of these projects provide
water for saltwater barriers to protect aquifers against seawater intrusion (Table 17). Since
membrane filtration is mandatory for all projects that inject recycled water, all of these four
projects use microfiltration and reverse osmosis.
52
Table 17: Projects Using Recycled Water for Groundwater Recharge Via Injection
S.No. Project Name Amount Recycled
(Acre-
Feet/Year) a
No. of injection
wells
Notes
1. West Coast Basin Saltwater Barrier
14,000 153 The recycled water for the West Coast Barrier is treated by the West Basin Municipal Water District Edward C. Little Water Treatment Facility. The facility can provide up to 75% of the water injected into the West Coast Basin Barrier. An increase up to 100% is planned. The facility produces softened Reverse Osmosis water which is secondary treated wastewater purified by micro-filtration (MF), followed by reverse osmosis (RO), and disinfection for groundwater recharge (West Basin Municipal Water District, n.d.).
2. Alamitos Saltwater Barrier
3,360 43 Recycled water for the Alamitos Barrier is produced by Water Replenishment District of Southern California (WRD)’s Leo J. Vander Lans Water Treatment Facility. This treatment plant can provide up to 50% of barrier water with recycled water. The remainder water for the barrier is imported. The facility receives tertiary-treated water from the Sanitation Districts of Los Angeles County and provides advanced treatment that includes microfiltration, reverse-osmosis, and ultraviolet light.
3. Dominguez Gap Barrier Project (DCBP) or Harbor Recycled Water Project
5,600 94 This project uses recycled water from the City of Los Angeles Department of Water and Power (LADWP)’s Terminal Island Treatment Plant (TITP) Advanced Water Treatment Facility. The plant is permitted to provide up to 5 million gallons per day (mgd) or 5,600 AFY, or 50% of the total barrier supply, whichever is less. The water is treated with microfiltration, reverse osmosis, and chlorination before being injected.
4. Orange County Groundwater
72,000 36 Approximately 30 MGD of the GWRS facility treated water is used for injection
53
S.No. Project Name Amount Recycled
(Acre-
Feet/Year) a
No. of injection
wells
Notes
Replenishment System (GWRS); Spreading/Injection
into the Talbert Barrier. Unlike other barrier projects in Southern California, 100 percent GWRS water is able to be used for injection into the seawater intrusion barrier without blending with other sources. Water at the GWRS facility is treated using microfiltration, reverse osmosis (RO) and ultraviolet (UV) disinfection with hydrogen peroxide.
a The water may need to be blended with other sources prior to recharge. The recycled amount estimates may change
depending on how much water is needed for barrier projects in future.
Sources:
Amount Recycled: (Sanitation Districts of Los Angeles County, 2011)
Number of injection wells (For projects 1,2,3): (Johnson, 2007)
Number of injection wells (For project 4): (Orange County Water District, n.d.)
Recycled water treatment and facility details (For projects 1,2,3) unless otherwise indicated: (Water Replenishment District of Southern California, 2011)
Recycled water treatment and facility details (For project 4): (Groundwater Replenishment System (GWRS))
A few planning stage projects are also assessing the feasibility of using recycled water for
groundwater recharge via injection (Table 18).
Table 18: Planned Projects Using Recycled Water for Groundwater Recharge Via Injection
S.No. Project/Agency Name
Amount Recycled
(Acre-Feet/Year)
No. of injection
wells
Notes and Sources
1. Camp Pendleton 435-870 12 The project will provide protection against salt water intrusion in the Lower Ysidora Sub-basin. Pilot testing was completed in 2012. (RMC Water and Environment, 2012 (Revised 2013)).
2. City of San Buenaventura
4000-7000 3-5 wells capable of sustained injection rates of between 2,500 to
The potential groundwater recharge reuse project (GRRP) in Mound Groundwater Basin will be used to store and reuse highly treated recycled water for Indirect Potable Reuse (IPR). The advanced treatment will involve desalination through a membrane process, advanced oxidation, and
54
S.No. Project/Agency Name
Amount Recycled
(Acre-Feet/Year)
No. of injection
wells
Notes and Sources
4,340 gpm
ultraviolet light (Hopkins Groundwater Consultants, Inc., 2013).
3. City of Oxnard’s Groundwater Recovery Enhancement and Treatment Program (GREAT Program). Program’s partners are United Water Conservation District (UWCD) and the Fox Canyon Groundwater Management Agency (FCGMA).
Ultimate plant capacity is 25 mgd
Design and permitting of pilot injection wells system is underway.
The Advanced Water Purification Facility (AWPF) and recycled water membrane treatment facility will provide high-quality water for groundwater injection and use as a seawater intrusion barrier (in the south Oxnard Plain) as well as for other uses including industrial processes and irrigation (Watersheds Coalition of Ventura County, 2006).
Because of the higher treatment costs associated with direct well injection of recycled water,
majority of the planned groundwater recharge reuse projects are expected to use surface
spreading rather than injection wells for groundwater recharge of recycled water (Sanitation
Districts of Los Angeles County, 2011). Therefore, statewide hydropower generation potential
from injecting recycled water for groundwater recharge is concentrated in a few regions of
Southern California and as with ASR and APH projects, this potential is constrained by
hydrogeological, site specific and operational parameters11.
4.4 Demand Response Potential of Groundwater Banks Reducing groundwater usage provides a substantial opportunity to reduce water-related energy
consumption of IOU energy (GEI Consultants/Navigant Consulting, Inc., 2010). Likewise,
“demand response”, that is, the ability to shift groundwater pumping from peak hours to non-
peak hours can reduce peak energy requirements and contribute towards overcoming the
barriers to renewable penetration. Water storage can be used to shave off more than one-third
of the peak load associated with groundwater use (California Energy Commission, 2005).
Having an onsite surface reservoir allows the water agencies or irrigation districts to pump
groundwater during off-peak hours and store it for use during on-peak hours. It is common for
many irrigation districts in California to have regulating reservoirs with volumes typically
11 One of these parameters is head loss or pressure loss. There used to be power generating stations at Water Replenishment District of Southern California (WRD) saltwater barrier facilities when the pressure of imported water (which is used for blending with recycled water) was sufficiently high. Energy generation has been discontinued however because of current low flows and reduced pressures (Ted Johnson (Chief Hydrogeologist, WRD), personal communication (EPC 15-049 Technical Advisory Committee Meeting), November 17, 2016).
55
ranging from 50,000 cubic meters (~ 40 AF) to 320,000 cubic meters (~260 AF) (Irrigation
Training and Research Center (ITRC)). Peak load curtailment and generation projects at several
water agencies including groundwater banking agencies such as North Kern Water Storage
District (NKWSD) and Berrenda Mesa Water Storage District have been funded with successful
results (Irrigation Training and Research Center (ITRC), 2005). Additionally, groundwater banks
that involve a significant pumping lift to deliver the extracted groundwater offer a unique
opportunity to combine demand response capabilities of pumping plants and well pumps at a
single site.
4.4.1 Peak Energy Requirements at Groundwater Banks
While pumped storage and associated peak hour generation benefits can potentially occur in all
hydrological year types, demand response benefits at groundwater banking projects will occur
largely in dry years since that is when most groundwater banking projects recover banked
water for delivery to partners or customers. The electric demand to pump the stored water
from a groundwater bank for delivery to participating agencies can be significant and add
considerably to the daily and seasonal peak summer loads. Therefore, groundwater banking
projects with demand response capability can decrease peak energy requirements which
opportunity has been recognized in earlier studies (Irrigation Training and Research Center
(ITRC), 2003). The facilities used to provide energy storage and peak energy generation at
groundwater banks can also be used for demand response. As with pumped storage, in most
cases only minor modifications to existing operations will be needed to enable shifting the
pumping demand out of the peak hours.
4.4.2 Demand Response Potential associated with Well Pumps
This study focuses on the demand response potential of relatively large groundwater banking
agencies that are likely to have clusters of high production wells. Though demand response can
be implemented at smaller agencies, data gaps and the scope of this study necessitate that
evaluation be restricted to large groundwater banking operations where closely located high
pumping capacity wells make the water storage and demand response practical and cost-
effective. This approach gives a preliminary estimate of statewide demand response potential
which in conjunction with the pumped storage and peak energy generation assessment
provides useful insights about the potential of groundwater banks to meet grid needs.
Since there is no statewide database providing information about well density or well pump
power consumption at various groundwater banks, groundwater banking agencies that are
likely to have clusters of wells were identified using the recovery volumes from the master
database (Antelope Valley Water Storage (AVWS), 2016) submitted with this report. The selected
groundwater banking projects have annual recovery volumes in thousands of acre-feet at a
minimum. The results from the literature review conducted for the Aquifer Pumped Hydro
(APH) and the statewide survey responses for the two pumped storage technologies were also
used to provide information on the number of wells and pumping capacity for selected
groundwater banking agencies. This information was compared to the pumping capacity
56
estimates derived from the recovery volumes to ensure that the assumptions do not result in an
overestimation of the demand response potential.
Figure 14 shows the monthly groundwater production profiles for selected hydrologic regions
where majority of large groundwater banking projects are situated. These regions include
Tulare Lake, San Joaquin River, and Sacramento River hydrologic regions which together
comprise what is commonly referred to as the Central Valley region of California. On average,
approximately 76% of the total groundwater pumped statewide every year is used to meet
agricultural demands (State of California Natural Resoures Agency, Department of Water
Resources , April 2015). Unlike urban groundwater use, agricultural groundwater use varies
considerably during the year (Figure 14). Seasonal demand response potential is therefore also
higher for agricultural sector. Central Valley has several large irrigation districts, many of
which have onsite groundwater banking operations as shown in Appendix F). Consequently, this
region has the highest groundwater pumping use (State of California Natural Resoures Agency,
Department of Water Resources , April 2015) and demand response potential as well as the
highest groundwater storage capacity (Table 19).
57
Figure 14: Monthly Groundwater Production (taf) by Hydrologic Region and Type of Use
taf= thousand acre-feet
Statewide, only 2% of the groundwater extracted on an average annual basis is used for managed wetlands (State of
California Natural Resoures Agency, Department of Water Resources , April 2015). For the purposes of this analysis, it is
assumed that no groundwater is pumped for managed wetlands use and all the extracted groundwater is used to meet Ag
or Urban demands.
Agricultural water demand is projected to decrease in the South Coast hydrologic region (California Department of Water
Resources, 2013). For this analysis, percentage of groundwater used for agriculture is assumed to be negligible (~0 AF) for
the South Coast hydrologic region.
Sources:
Average Annual Groundwater Supply by Hydrologic Region and Type of Use (State of California Natural Resoures Agency, Department of Water Resources , April 2015)
Monthly Profiles for Groundwater Production (%) by Hydrologic Region and Type of Use (GEI Consultants/Navigant Consulting, Inc., 2010)
58
Table 19: Demand Response Potential of Well Pumps at Groundwater Banking Projects
Hydrologic Region Total Storage Capacity (MAF) of listed projects
Demand Response Potential (MW) of listed projects
Central Coast Hydrologic Region 5.9 99South Coast Hydrologic Region Colorado River Hydrologic Region South Lahontan Hydrologic Region San Joaquin River Hydrologic Region
0.3 2
Sacramento River Hydrologic Region
2.36 2
Tulare Lake Hydrologic Region 11.48 115San Francisco Bay Hydrologic Region
0.23 2
Total ~20 ~220
Sources:
The storage capacity is from the master list of groundwater banking projects which was also one of the study deliverables (Antelope Valley Water Storage (AVWS), 2016)
Demand Response Potential estimates are provided in Appendix F.
4.4.3 Demand Response Potential associated with Pump Station(s)
Any groundwater bank that has area for siting upper and lower reservoirs and relies on
pumping plants to get water into or out of the bank can potentially provide demand response
benefits by shifting peak summer demand to off-peak hours in an extraction year. Assuming
the statewide PHPS potential is 44 MW (Table 16), groundwater banks across the State can free
up more than 44 MW in cumulative peak capacity (The PHPS assessment for Willow Springs
Water Bank (WSWB) indicates that for a given PHPS lift, the power demand to pump water to the
upper reservoir is likely higher than the power produced during the generation cycle). A
project’s operational pumping capacity is the key indicator of its demand response capability.
4.5 Regulatory Considerations Current and future regulatory criteria will also impact the technical and economic feasibility of
pumped storage. As discussed in Chapter 2 the low round-trip efficiency makes APH
deployment on a large scale unlikely. The success of APH is likely only at groundwater banking
sites that currently operate as ASR projects and are therefore located in areas of relatively high
transmissivity. Assuming that the APH deployment is restricted to sites with active ASR
operations, permitting requirements would be minimal since an existing ASR project will
typically have approved injection and extraction operations that have been evaluated for
compliance with water quality and other regulatory criteria. For these sites, permitting would
generally only be needed to equip the existing wells with turbines to generate power and to
obtain approval for utility interconnection. Permitting requirements will be more extensive for
sites that do not have active ASR activities. At the very minimum, these projects will have to
meet Regional Water Quality Control Board (RWQCB) requirements to pump, store, and inject
groundwater.
59
For Peak Hour Pumped Storage (PHPS), both upper and lower reservoirs will need to be covered
and lined to keep out tumbleweeds and dust. Floating covers could be used for the purpose. For
full-scale implementation of a PHPS project, a Federal Energy Regulatory Commission (FERC)
approval or “Conduit Exemption” and an environmental document such as Supplemental
Environmental Impact Report (EIR) or Subsequent EIR will be needed at a minimum. An
Environmental Impact Statement (EIS) may also be required if a FERC Traditional Review
process to obtain a license has to be implemented.
Appendix G lists additional permits and registrations, some or all of which may be needed to
test and deploy pumped storage at a groundwater banking project. Compliance with regulatory
criteria will ensure that any negative environmental impacts that may result from
implementation of pumped storage at groundwater banks are avoided or suitably mitigated.
4.6 Template to Assess Pumped Storage Potential The objective of the template is to provide a decision-making tool to assess current and future
groundwater banking operations for energy storage and demand response potential. The
template walks the user through a series of preliminary questions and calculations to
determine a site’s technical and economic viability for pumped storage implementation. The
template incorporates criteria pertaining to a site’s physical and operational parameters,
preliminary regulatory requirements and economics (including threshold generation capacity
(MW), and value of on-peak energy generation and any other grid benefits) to provide a
conceptual estimate of a site’s feasibility for APH or PHPS. The template and its accompanying
documentation submitted with this report describe the criteria in detail.
The template also includes an assessment of a project’s potential to participate in a demand
response program. Demand response benefits have traditionally come from turning off the
pumps at the pumping plant and groundwater well pumps during the peak hours but
increasingly are looking at increasing demand during renewable overgeneration hours. The
demand response program will be most effective in places where high capacity wells are located
close together so as to require a single reservoir for storing the water pumped during off-peak
hours. For evaluation of demand response potential, appropriate criteria including number of
additional wells that may be needed have been incorporated in the template.
The developed template may be used to identify candidate sites for pilot testing of APH and
PHPS. Along with the technical criteria, the template also includes regulatory costs for pilot
stage projects. These costs will impact the economics of future pilot stage projects and have
also been considered in this analysis.
4.7 Summary of Statewide Analysis At the outset of the study, it was presumed that the available underground storage capacity in
the State is a good indicator of the undeveloped statewide pumped storage potential at
groundwater banks (Antelope Valley Water Storage (AVWS), 2015). The State’s total
groundwater banking capacity is estimated to be 22 MAF (Lund, Munevar, Taghavi, Hall, &
60
Saracino, 2014) and WSWB capacity is 2.3% (1/44th) to 4.5% (1/22nd) of this total12. The
statewide pumped storage potential extrapolated as a function of the storage capacity using the
initial pumped storage estimates (6 MW to 13 MW) for WSWB resulted in an order-of-magnitude
estimate of 70 MW to 140 MW of statewide storage benefits (assuming either energy storage
system is applicable at 50% of groundwater banks). This indicated that either pumped storage
concept has the potential to meet 1% to 2% of the State’s storage needs (assuming the State
needs 6000 MW of storage to meet the 50% renewable penetration goal by 203013 )
A key goal of the statewide analysis was to determine more precise estimates for the statewide
pumped storage potential at groundwater banks. The following key findings (discussed in
detail in the previous sections of this report) indicate that the estimated statewide pumped
storage potential (44 MW) at groundwater banks is at the low end of the initial estimates:
1. The high round-trip losses associated with APH have a considerable impact on the statewide
pumped storage potential of the well field at groundwater banks. Hydropower generation using
the well field will likely be limited to sites that currently use dual injection/extraction wells
(ASR projects).
2. The statewide power generation potential at groundwater banks that use recycled water for
groundwater recharge is low since the injection method for recharge requires advanced water
treatment. Therefore, majority of the groundwater recharge reuse projects use surface
spreading instead of subsurface injection as the choice method of recharge. Therefore, these
projects typically do not have a well field that has power generation potential. These recycled
water projects also have negligible potential for PHPS since elevation differences from
treatment facilities to the recharge basins are unlikely to be significant.
3. Demand response potential of groundwater banking projects is significant and can reduce
peak hour demand associated with well pumps by 220 MW during dry years. Additional peak
demand reduction may result if groundwater banking projects (like WSWB) have a substantial
lift to the delivery conveyance. These estimates assume that most of the large groundwater
banking projects have the operational flexibility to shift the pumping demand and vary water
delivery amounts. Costs associated with additional surface storage capacity and wells are
included in the costs and benefits analysis of statewide demand response potential at
groundwater banks. PHPS and APH templates can be used to determine the total demand
response potential at a particular groundwater banking project.
12 Although the 2006 EIR for WSWB approved the total bank volume of 500,000 AF, later groundwater modeling results indicate that the bank can store up to 1,000,000 AF of water with put and take capacities of 250,000 AFY. Using 1,000,000 AF estimate for WSWB’s groundwater banking capacity provides conservative estimates for statewide pumped storage potential.
13 California is likely to require between 3,000 MW to 4,000 MW of fast acting energy storage by 2020 to integrate the projected increase in renewable energy. The California 2030 Low Carbon Grid study projects need of 2550 MW to be built between 2020 and 2030 to enable 50% reductions in grid GHG emissions below 2012 levels by 2030 (57% renewable penetration by 2030). The baseline case in this study assumes 33% renewable penetration (No change from 2020 levels of renewable penetration). Therefore, by 2030, CA is likely to need roughly 6000 MW of storage to meet renewable integration goals. (California Energy Commission, 2015) (National Renewable Energy Laboratory (NREL), 2014).
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Information gaps relating to the statewide peak power demand data for well pumps, typical
well densities at groundwater banking projects, elevation differences, and pipeline length will
need to be addressed to obtain more precise estimates of pumped storage and demand
response capabilities of groundwater banks.
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CHAPTER 5: Economics Evaluation
As part of this project, Water & Energy Consulting (WEC) was retained to evaluate the value of
pumped storage at groundwater banks. Energy storage is recognized as being critical to
California’s energy future to accommodate intermittent renewable generation (California ISO,
2014)). Energy storage can provide two types of services: long duration services, for example
charging during periods of renewable overgeneration and generating during other periods, and
short duration services, such as ancillary services (Mathias, Doughty, & Kelly, 2016). This
project assesses both these attributes. The economics evaluation was submitted in two
technical memorandums (House L. W., 2017 a; House L. W., 2017 b) to the California Energy
Commission. This chapter contains excerpts from these memorandums and lays out the
characteristics of pertinent markets/services, and the economics of pumped storage at Willow
Springs Water Bank (WSWB) and at groundwater banks around the State.
5.1 Participation in ISO Markets The California Independent System Operator (California ISO) provides markets for various
services and access to the transmission grid. California ISO currently runs three primary
wholesale energy markets: Day-Ahead, Real-Time, and Ancillary Services.
5.1.1 Day-Ahead market
The Day-Ahead market is made up of three market processes that run sequentially. First, the
ISO runs a market power mitigation test. Bids that fail the test are revised to predetermined
limits. Then the integrated forward market establishes the generation needed to meet forecast
demand. And last, the residual unit commitment process designates additional power plants
that will be needed for the next day and must be ready to generate electricity. Market prices set
are based on bids. The Day-Ahead market opens for bids and schedules seven days before and
closes the day prior to the trade date. Results are published at 1:00 p.m.
5.1.2 Real-time market
The Real-time market is a spot market in which load serving entities can buy power to meet the
last few increments of demand not covered in their day ahead schedules. It is also the market
that secures energy reserves, held ready and available for ISO use if needed, and the energy
needed to regulate transmission line stability. The market opens at 1:00 p.m. prior to the
trading day and closes 75 minutes before the start of the trading hour. The results are
published about 45 minutes prior to the start of the trading hour. The Real-time market system
dispatches power plants every 15 and 5 minutes, although under certain grid conditions the
California ISO can dispatch for a single 1-minute interval.
63
5.1.3 Ancillary service market
Ancillary services are energy products used to help maintain grid stability and reliability. These
services are functions performed by electrical generating, transmission, system-control, and
distribution system equipment and people to support the basic services of generating capacity,
energy supply, and power delivery. The Federal Energy Regulatory Commission (FERC 1995)
defined ancillary services as “those services necessary to support the transmission of electric
power from seller to purchaser given the obligations of control areas and transmitting utilities
within those control areas to maintain reliable operations of the interconnected transmission
system.” There are four types of ancillary services products currently procured: regulation up,
regulation down, spinning reserve and non-spinning reserve. Regulation energy is used to
control system frequency, which must be maintained very narrowly around 60 hertz, and varies
as generators change their energy output. Resources providing regulation are certified by the
ISO and must respond to automatic control signals to increase or decrease their operating
levels depending upon the need. Spinning reserve is standby capacity from generation units
already connected or synchronized to the grid and that can deliver their energy in 10 minutes
when dispatched. Non-spinning reserve is capacity that can be synchronized to the grid and
ramped to a specified load within 10 minutes.
Generators participating in the ISO markets are limited to one megawatt or more. Their ability
to participate in the various markets is limited by their configuration (various ancillary service
markets have response/performance requirements) and their operation (many of the ancillary
services markets require direct ISO control of the generator).
5.1.4 Load Participation
Load can also participate in California ISO markets. California ISO rules allow load and
aggregation of loads capable of reducing their electric demand to participate as price
responsive demand in the ancillary services market and as curtailable demand in real-time
markets. Load can participate in some ISO markets via a Proxy Demand Resource (PDR) or via a
Reliability Demand Response Resource (RDRR). PDR and RDRR only allow for load curtailment,
not load consumption or the export of energy to the grid.
Proxy Demand Resource (PDR) is a participation model for load curtail introduced in 2010 to
increase demand response participation in the ISO’s wholesale Energy and Ancillary Services
markets. PDR helps in facilitating the participation of existing retail demand response into
these markets: Day-Ahead, Real-time, Spinning and Non-Spinning Reserves like a generator
resource, but it cannot ever inject energy into the grid. PDR can only be dispatched in one
direction – to reduce load.
Reliability Demand Response Resource (RDRR) is a product created to further increase demand
response participation in the ISO markets by facilitating the integration of existing emergency-
triggered retail demand response programs and newly configured demand response resources
that have reliability triggers and desire to be dispatched only under certain system conditions.
RDRR may participate in the Day-Ahead and Real-time markets like a generator resource, but
64
may not submit Energy Self-Schedules, may not Self-Provide Ancillary services, and may not
submit Residual Unit Commitment (RUC) Availability or Ancillary service bids.
Electricity storage can participate in the ISO markets also. A storage device could participate
using the ISO's non-generating resource (NGR) participation model. The main difference of
NGR compared to a generator is that the NGR can have negative output (absorbing electricity
from the grid). Additionally, NGRs are ISO metered entities requiring them to comply with ISO
metering and telemetry requirements. All utility interconnection requirements would need to
be met which may include the need to obtain a Wholesale Distribution Access Tariff (WDAT)
interconnection, similar to any other generator connected at the distribution level that
participates in the wholesale market.
5.1.5 Other Markets/Services
There is a California Public Utilities Commission (CPUC) proceeding (R.15-03-011) and an ISO
stakeholder initiative on Energy Storage and Distributed Energy Resources that is investigating
additional markets/service for energy storage and distributed energy resources. Table 20
provides a summary of the reliability and non-reliability services that are being investigated in
these proceedings.
Table 20: Storage Reliability Services and Non-Reliability Services
Domain Reliability Services Non-Reliability Services
Customer None TOU bill management; Demand charge management; Increased PV self-consumption; Back-up power
Distribution Distribution capacity deferral;
Reliability (back-tie) services2
Voltage support;
Resiliency/microgrid/islanding
Transmission Transmission deferral; Inertia;
Primary frequency response;
Voltage support; Black start
None
Wholesale Market Frequency regulation; Spinning
reserves; Non-spinning reserves
Imbalance energy
Resource Adequacy Local capacity; Flexible capacity System capacity
Source: (California Public Utilities Commission, 2017; House L. W., 2017 b)
It should be emphasized that there are a number of services listed in Table 20 for which there
is currently no existing market (back-tie services, inertia, primary frequency response, and
resiliency). For reliability services, there can be reliability impacts to the system if the resource
does not follow instructions from the ISO or utility distribution company (UDC).
65
Groundwater bank energy storage systems could participate as either a generator or as a
demand (load) in the ISO markets, but not all markets/services are available to both operations.
A summary of the available and potential markets and services as applicable to groundwater
pumped storage projects is provided in Table 21.
Table 21: Potential Markets and Services for Groundwater Bank Pumped Storage Operation
Market or Service
Groundwater Bank Operation
Comments
Bulk Energy Supply (day ahead, real time, retail energy shift)
Generation
Load
If there is water available at elevation to run through hydroelectric generators
If operating via PDR or RDRR
Frequency Regulation Generation (currently)
Load (theoretically as dedicated Demand Response)
If generation configured properly, is operating and under ISO Automatic Generation Control (AGC)
If configured properly, load operating and dedicated to ISO control
Spinning Reserves Generation
Load
If generation configured properly, is operating and under ISO control
If operating via PDR
Non-Spinning Reserves Generation
Load
If generation configured properly
If operating via PDR
Regulation Energy Management
Generation
Load (theoretically)
If configured properly and participating in ISO regulation up/down markets
If configured properly and participating in ISO regulation up/down markets
Flexible Ramping Generation
Load (theoretically)
If configured properly.
66
Market or Service
Groundwater Bank Operation
Comments
If configured properly and allowed to provide service
Investment Deferral Generation
Load
Generators or reduction in load that is capable of reliably and consistently reducing net loading on desired distribution infrastructure.
Reactive Power/Voltage Support
Generation
Load
If configured properly and operated under ISO control
Not applicable.
Resource Adequacy Generation
Load
If configured and operated properly and participates in ISO markets
Demand Response Generation
Load
Not applicable
Depends upon ability to curtail/shift load
Black Start Generation
Load
Only if there is water available at elevation to run through hydroelectric generators and configured for black start.
Not applicable.
Source: (House L. W., 2017 b)
A key point to remember from Table 21 is that all these markets/services have specific
performance requirements which may not be compatible with groundwater banking operations.
The primary purpose of groundwater storage banks is to store water and the operation of a
pumped storage project cannot interfere with that water storage priority. A pumped storage
addition will need to be carefully configured to provide some of these services without
compromising the water bank operation. Water bank operator may be reluctant to turn
operation of their facility over to the ISO in order to participate in some ancillary markets.
For example, Resource Adequacy (RA) capacity is classified as system, local, or flexible. The
rules for system and local RA define the qualifying capacity (QC) of a storage resource to be the
maximum discharge rate the resource can sustain for four hours14. If a storage resource is 14 A storage resource that can store 4 MWh of energy would typically be able to sustain a 1 MW discharge rate for 4 hours and would therefore qualify to provide 1 MW of system or local RA capacity.
67
counted toward a load serving entity’s resource adequacy obligation, then it must participate in
the wholesale market and be subject to a must-offer obligation. A must-offer obligation
requires the resource to participate in the market during specific time periods and with specific
rules, it is a requirement to bid or schedule the capacity into the ISO’s Day-Ahead and Real-time
markets in accordance with specific ISO tariff provisions, and to be able to perform to fulfill its
ISO schedule or dispatch instructions. A groundwater pumped storage facility would have to
maintain sufficient water in elevated storage for 4 hours of operation at all times to qualify for
Resource Adequacy.
5.2 Economics Analysis Approach The economic feasibility of pumped storage at WSWB was determined and used as a baseline to
extrapolate the value of pumped storage to the groundwater banking sites around the State
where pumped storage appears to be technically feasible. The potential benefits and their
corresponding economic values have also been incorporated into the two pumped storage
templates which can be used to evaluate the economics of pumped storage at a particular
groundwater banking site.
5.3 Economic Feasibility at Willow Springs Water Bank Pumped storage can potentially occur in all hydrological year types (Figure 9). However, for
simplicity of economics analysis, it is assumed that to be compatible with groundwater banking
operations, pumped storage will occur only in the idle (or neutral) year type i.e., when no
recharge or extraction activities are taking place. In a wet year, the Bank will be recharging the
water year-round and will be operated in the hydropower generation mode. In a dry year it will
be extracting or pumping the water year-round and therefore, has the potential to provide
demand response. Additionally, while the technical analysis is based on the planning
documents for WSWB (GEI Consultants, Inc., 2016) which indicate an average pumping demand
of 225 kW/well (300 hp/well), for economics analysis, 278 kW/well (about 375 hp/well) has
been used which is a conservative estimate and includes 20% for hydrogeologic uncertainty
related to drawdown.
5.3.1 Operating Scenarios
Pumped storage will supplement the hydropower generation and demand response potential of
WSWB and will enable use of the Bank’s facilities even in the absence of recharge and recovery
activities. The benefits to the grid were assessed based on the operating scenarios which will
determine whether the Bank operates as a hydroelectric generator, a pumped storage facility or
as a load.
Recharge Year (wet): A recharge year involves up to 385 cubic feet per second (cfs) of
recharge. That enables a total recharge of 280,000 acre-feet per year to the water bank.
250 cfs will be used to generate electricity 24 hours a day and 135 cfs will bypass the
turbine. The estimated occurrence rate is 1 year in 3 based on historical record (32%).
Idle (Neutral) Year: An idle year does not have any predetermined recharge or extraction
activity. 250 cfs of water will be used to generate electricity for the 5 hours daily from
68
the upper reservoir. The water will be replaced over the other 19 hours. The estimated
occurrence rate is 1 year in 3 based on the historical record (33%).
Extraction Year (dry): Withdrawals of water from the water bank will occur in a dry year. 250
cfs will be pumped back to the California Aqueduct and 60 cfs will be delivered to the
Antelope Valley-East Kern Water Agency potable system for exchange or to the
Aqueduct. The total extraction requirement is 310 cfs. The estimated occurrence rate is
1 year in 3 based on historical record (35%).
These operating scenarios are illustrated in Figure 15 which shows WSWB being operated to
provide hydropower generation (in wet year), PHPS (in idle year), and demand response (5 hours
daily curtailment on summer weekdays in dry year).
Figure 15: Operating Configurations for WSWB by Year Type
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5.3.2 StorageVET™ Model
Water & Energy Consulting (WEC) used the Storage Value Estimation Tool (StorageVET™) to
evaluate the value of the two pumped storage technologies at WSWB (House L. W., 2017 a).
StorageVET™ is publicly available via the EPRI website (http://www.storagevet.com/) and allows
consistent estimation of benefits and costs of various energy storage projects.
5.3.3 Aquifer Pumped Hydro (APH) Economics
Aquifer Pumped Hydro at WSWB will require the addition of reversible pump turbines to
existing recovery wells. Assuming the other components (such as surface reservoir) are part of
the WSWB project, the only additional capital cost will result from the addition of the electrical
and mechanical Package ($0.30 M/well).
Neutral year operation of APH was assessed as an energy storage project in StorageVet (Table
22), using 2015 SCE DLAP (Default Load Aggregation Point) prices. (DLAP reflects the costs SCE
avoids in procuring power during the time period.) The operation was evaluated in the Bulk
Energy Market (Day-Ahead Energy Market) generating when electricity prices were high, and
pumping water from the ground when prices were low. It was not evaluated in either the
Flexible Ramping or the Demand Response markets because participation in both these markets
necessitates that the surface reservoir be full. As discussed in Chapter 2, the round-trip
efficiency of APH at WSWB is so low (22%) that it was impractical to keep the surface reservoir
full. This operational characteristic prevents the project from providing these additional
services.
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Table 22: StorageVET™ Technology Parameters Used for WSWB APH Simulation
Parameter Value
Pumping Capacity [kW] a 17,236 kW
Generating Capacity [kW] 3,700 kW
Energy Storage Capacity [kWh] 18,500 kWh (3.7 MW*5 hours)
Upper Limit, Operational State of Charge [%] 100
Lower Limit, Operational State of Charge [%] 0
Pumping (Charge) Efficiency [%] 0.416
Generating (Discharge) Efficiency [%] 0.518
Max Discharge Ramp [kW / min] 1,000
Annual O&M b 0
Capital Cost c $18.6 M
a Assuming power required for pump mode is 278 kW/well (Table 5).
b Assuming operating cost is covered by existing water bank operations.
c For 62 wells, the capital cost would be $18.6M to implement 3.7 MW of hydropower generation ($5,100/KW) (Table 8).
Source: (House L. W., 2017 a)
Even in the Day-Ahead Energy Market the project has limited potential for participation with
the result that the APH operation virtually never runs – the round-trip efficiency is so low there
is rarely enough of a daily price spread to economically pump and generate. Therefore, the Net
Present Value is a large negative number (Table 23).
Table 23: Economics of APH Operation at WSWB
Value
Benefit MARKET: Day Ahead Energy $4,044 per year
Cost Debt Service -$1,599,072 per year
O&M 0
Net Present Value (20 year, 6% discount rate) -$18,294,846
StorageVet Simulation for APH at WSWB using 2015 SCE DLAP prices
Source: (House L. W., 2017 a)
During wet years the water bank is doing recharge around the clock. However, the well field
cannot operate as a constant year-round generator during a wet year. Some of the recharge
71
water (State Water Project (SWP) water) could potentially be injected into the ground; however,
because the recharge would be by injection instead of percolation using spreading grounds, the
project would need to meet additional the Regional Water Quality Control Board (RWQCB) water
quality criteria. This requirement would increase the capital cost of the project and make it
infeasible.
5.3.4 Peak Hour Pumped Storage (PHPS) Economics
PHPS at WSWB will require the addition of an upper reservoir and two 3.4 MW 5-jet Pelton
Wheel turbines.
5.3.4.1 Neutral Year (33% probability) – Pumped Storage Mode
Neutral year operation of PHPS was assessed as a pumped storage project in StorageVet (Table
24) generating when electricity prices were high, and recharging water into the ground when
prices were low (5.2 MW generation, 10.1 MW demand for pump station use).
Table 24: StorageVET™ Technology Parameters Used for WSWB PHPS Simulation
Parameter Value
Pumping Capacity [kW] 10,124 kW
Generating Capacity [kW] 5,223 kW
Energy Storage Capacity [kWh] 26,000 kWh (5.2 MW*5 hours)
Upper Limit, Operational State of Charge [%] 100
Lower Limit, Operational State of Charge [%] 0
Pumping (Charge) Efficiency [%] 0.834
Generating (Discharge) Efficiency [%] 0.874
Max Discharge Ramp [kW / min] 1,000
Annual O&M $100,000
Capital Cost $7.9 M
Source: (House L. W., 2017 a)
The operation was evaluated using 2015 SCE DLAP (Default Load Aggregation Point) prices and
in the Day Ahead Energy Market. Since PHPS can provide generation during the morning and
evening ramp periods, and increased demand (load) during the afternoon periods to refill
storage reservoirs, it was evaluated for Flexible Ramping and Demand Response markets along
with Day Ahead Market (Table 25).
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Table 25: WSWB PHPS Operation (Neutral Year – 33% Probability)
Market Annual Value
Day Ahead Market (Energy) $94,852
Flexible Ramping $384,637
Demand Response $384,637
Total $791,079
StorageVet Simulation for PHPS neutral year at WSWB using 2015 SCE DLAP prices. Numbers are not rounded to reflect
model results.
Source: (House L. W., 2017 a)
5.3.4.2 Wet Year (32% probability) – Hydropower Generation Mode
During wet years, the water bank is storing water and will recharge water into the Bank’s
percolation ponds for storage at a constant flow of 250 cfs. Therefore, the Bank can use PHPS
facilities (the two 3.4 MW Pelton Wheel turbines) to operate as a year-round hydroelectric
generator during a wet year. For this scenario, the project was evaluated as a 5.2 MW
hydroelectric generator operating 24 hours a day. 2015 SCE DLAP hourly prices were used in
the evaluation. Table 26 shows the annual benefit of WSWB operating as a hydroelectric
generator during wet years. There is additional flexibility possible with this technology. The
Bank could use the upper reservoir component of PHPS to curtail generation for 5 hours per
day during the afternoon period when there is a surplus of renewable generation.
Table 26: WSWB Hydroelectric Generator Mode (Wet Year – 32% Probability)
Market Annual Value a
Day Ahead Energy $1,386,330
a 5.2 MW operating 24/7, priced at 2015 SCE DLAP prices, assuming no curtailment or load following.
Source: (House L. W., 2017 a)
5.3.4.3 Aggregate Summary for PHPS and Hydropower generation at WSWB
PHPS at WSWB was evaluated for neutral year (Table 25). In the pumped storage configuration,
depending on the time of day, the Bank will serve as a load or a generator. PHPS facilities can
also be used to generate electricity year-round during a wet year (Table 26) and in this scenario,
the Bank will function as a hydropower generator. Table 27 provides a probability weighted
summary of the cost effectiveness of integrating PHPS and hydropower generation to the
existing WSWB configuration. The cost of the necessary enhancements to the existing WSWB to
develop a PHPS project is estimated at $7.9 million. The NPV (net present value) of the
73
probability weighted operation of this facility is a negative $0.99 million for a 20-year
investment horizon15.
Table 27: Cost effectiveness of PHPS and Hydropower Generation at WSWB
Year Type Probability Operated As Annual Value
Wet 32% Generator $1,386,330
Neutral 33% Pumped Storage a $791,079
Probability Weighted Annual Benefit $704,682
Annual O&M -$100,000
Annual Debt Service ($7.9M at 6% for 20 years) -$691,243
Annual Net Benefit -$86,561
NPV of PHPS and Hydropower Generation -$992,853
a Cost-Effectiveness evaluation based on standard protocol (DNV-GL Energy and Sustainability, 2013).
Source: (House L. W., 2017 a)
5.3.5 Dry Year (35% probability) – Demand Response
Demand response is the ability to reduce or vary electricity use when needed. This is possible at
WSWB in an extraction or dry year and will reduce load during the late afternoon ramping
period and evening peak. In a dry year WSWB will extract water and pump it to the California
Aqueduct. This year was evaluated for demand response (curtailing electricity use in response
to system needs). The electricity demand is continuous from groundwater pumping (17.2 MW)
plus power for the pump station (10.1 MW). Therefore, the project was evaluated as a 27.3 MW
continuous year-round load operating 24 hours a day, with the ability to be curtailed up to 5
hours per day for up to 320 hours per year.
Pumps at the pumping plant could be shut off for 5 hours a day during years that water is
being pumped back to the California Aqueduct. The demand response potential of the pumping
plant corresponds to the size of the pumps, or 10.1 MW. It can be realized by shutting down the
pumping to the Aqueduct for 5 hours a day. In addition, the 62 extraction wells (17.2 MW)
could be curtailed for those 5 hours also. To provide for this level of demand response two
additional extraction wells would need to be added to make up for the 320 hours annual
pumping curtailment16.
The project was evaluated for demand response using values from 2025 California Demand
Response Potential Study (Lawrence Berkeley National Laboratory, 2017). This study recognizes
three primary types of demand response: Shift, Shed, and Shimmy (Table 28).
15 Assuming no escalation annual benefits, a 20-year horizon, and a 6% discount rate.
16 Additional curtailment would require the addition of additional extraction wells.
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Table 28: Types of Demand Response
Service
Type
Description Grid Service
Products/Related Terms
Shift Demand timing shift
(day-to-day)
Flexible ramping DR (avoid/reduce ramps), Energy market price smoothing
Shed Peak load curtailment
(occasional)
CAISO Proxy Demand
Resources/Reliability DR
Resources; Conventional DR, Local Capacity DR, Distribution System DR, RA Capacity, Operating Reserves
Shimmy Fast demand response Regulation, load following, ancillary services
Source: (Lawrence Berkeley National Laboratory, 2017)
The Shift service type is demand response that moves load to desired times during the day,
increasing energy consumption during periods of the day when there is surplus generation, and
reducing consumption during periods of the day when there is excess load.
The Shed service type describes loads that can occasionally be curtailed to reduce customer
demand during peak net load hours.
The Shimmy service type involves using loads to dynamically adjust demand on the system to
alleviate ramps and disturbances at timescales ranging from seconds up to an hour.
Table 29 shows the annual benefit of WSWB providing demand response services during a dry
year.
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Table 29: WSWB Operated as a Continuous Load (Dry Year – 35% Probability)
Demand Response
Service
Market Value (low)
Market Value (high)
Unit WSWB Annual Value
(low)
WSWB Annual Value
(high)
Shed $4 $4 $/kW-year $109,200 $109,200
Shift $20 $52 $/MWh $174,720 $454,272
Shimmy – load following
$35 $45 $/kW-year $955,500 $1,228,500
Shimmy – regulation
$57 $98 $/kW-year $1,556,100 $2,675,400
Total $2,795,520 $4,467,372
WSWB dry year demand response simulation assumes availability of up to 5 hours of daily curtailment; 27.3 MW
curtailable up to 320 hours per year.
Source: (House L. W., 2017 a)
5.3.5.1 Adding dry year demand response to APH and PHPS
To complete operations analysis for all three year types, dry year demand response was added
to APH and PHPS (Table 30). Adding dry year demand response to neutral year PHPS and wet
year hydropower generation modes increases their NPV to almost $8 million, but is still not
enough to make APH cost effective. A summary of the operational modes for APH and PHPS
facilities and their corresponding services is given in Table 30.
Table 30: Comparison of WSWB APH and PHPS Characteristics and Analysis
WSWB Aquifer Pumped Hydro (APH)
WSWB Peak Hour Pumped Storage (PHPS)
Demand Response
Components needed Reversible pump-turbines, surface storage reservoir, aquifer is lower reservoir
Hydroelectric generator, upper and lower surface reservoirs
2 additional groundwater wells for 320 hours curtailment
Pumping Capacity 17.2 MW 10.1 MW 27.3 MW
Generating Capacity 3.7 MW 5.2 MW
Energy Storage
(5 hours of generation)
18.5 MWH 26.0 MWH Curtailable up to 320 hours per year
Pumping Efficiency 41.5% 83.4%
Generating Efficiency 51.7% 87.4%
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WSWB Aquifer Pumped Hydro (APH)
WSWB Peak Hour Pumped Storage (PHPS)
Demand Response
Round Trip Efficiency 21.6% 72.9%
Capital Cost $18.6M $7.9M $2.1M
Net Present Value (@6%, 20 years)
-$18.2M (generator operating in neutral
years)
-$0.9M (generator operating during wet and neutral year)
$9.1M (dry year)
Capital Cost with Dry Year Demand Response
$20.3M $10M
Net Present Value (@6%, 20 years) with dry year demand response
-$9.1M $8.1M
Markets/Services:
Day Ahead Hourly Market Yes Yes
Flexible Ramping No, response time too slow, operational parameters preclude
Yes
Demand Response Yes Yes
Real Time Energy Time Shift
No No
Retail Energy Time Shift No, lack of load on site No, lack of load on site
Frequency Regulation No, not configured for, wish to maintain local control of operations
No, not configured for, wish to maintain local control of operations
Spinning Reserve No, not configured for, wish to maintain local control of operations
No, not configured for, wish to maintain local control of operations
Non-Spinning Reserve No, not configured for, wish to maintain local control of operations
No, not configured for, wish to maintain local control of operations
Regulation Energy Management (REM)
No, not configured for, wish to maintain local control of operations
No, not configured for, wish to maintain local control of operations
Investment Deferral No. Area of WSWB is an unconstrained SCE area
No. Area of WSWB is an unconstrained SCE area
Reactive Power/Voltage Support
No, not configured for, wish to maintain local control of operations
No, not configured for, wish to maintain local control of operations
77
WSWB Aquifer Pumped Hydro (APH)
WSWB Peak Hour Pumped Storage (PHPS)
Demand Response
Resource Adequacy Capacity (RA)
No, expected operations preclude
No, expected operations preclude
Black Start No, not configured for No, not configured for
Source: (Water & Energy Consulting, 2017a)
As Table 30 shows, there are a multitude of ancillary services that could be possible using the
PHPS and APH facilities – if they were configured properly and if the water bank was willing to
turn over operational control of the facilities to the Independent System Operation (Frequency
Regulation, Spinning Reserve, Non-Spinning Reserve, Regulation Energy Management [REM],
Reactive Power/Voltage Support, and Black Start require the generation facilities to be under
ISO control). WSWB’s primary purpose is as a water storage facility and the Bank is therefore
reluctant to invest in the additional facilities necessary to perform these services or turn over
operation of the water bank to the ISO in order to participate in many of these markets.
Therefore, the ancillary services options for WSWB were limited.
5.4 Economic Evaluation for Statewide Pumped Storage at Groundwater Banks Pumped storage additions to existing groundwater banking facilities have the potential to
provide electrical grid benefits from 1) generation of electricity during period of high system
demand; 2) increase in pumping demand (load) during renewable overgeneration periods to
reduce the risk of overgeneration; 3) reduction of load during high system ramping
requirements and system demand; and 4) delivery of a plethora of ancillary services, depending
upon the configuration of the groundwater bank and its ability to cede operational control to
the ISO. Assuming that WSWB operations are typical of most groundwater banking projects, the
operating configurations and their associated costs and values identified for WSWB can be used
to evaluate economic feasibility of pumped storage, hydropower generation, and demand
response benefits at groundwater banks around the State.
5.4.1 Potential Markets and Services
As discussed in the preceding sections, a groundwater bank’s facilities (including additional
pumped storage facilities) can be configured to operate in different modes to participate in
markets applicable to pumped storage, hydropower generation and demand response. A
summary of the characteristics of these markets/services is provided in Table 31.
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Table 31: Potential Markets for Groundwater Bank Energy Operations
Market/Service Definition Time Period Applicable to Groundwater Bank Pumped
Storage Facilities
WSWB APH Simulation
WSWB PHPS
Simulation
Day Ahead Energy Time Shift
Hourly market energy prices established for the next day. Based upon unit commitment on the day prior to the actual operating day.
Hour In both generating and pumping mode.
Yes Yes
Real Time Energy Time Shift
The real-time market is a spot market in which utilities can buy power to meet the last few increments of demand not covered in their day ahead schedules.
15-minute procurement, 1 hour continuous requirement
In both generating and pumping mode.
No Yes
Retail Energy Time Shift
Hourly energy and demand prices based upon utility retail tariffs.
Hour If significant on-site electricity use
No No
Frequency Regulation
Maintaining the grid frequency within the given margins by continuous modulation of active power. Capacity that follows (in both the positive and negative direction) a 4-second ISO power signal.
Seconds Have to be operating and have special generation configuration for rapid response.
No No
Spinning Reserve
Spinning reserve is standby capacity from generation units already connected or synchronized to the grid and that can deliver their energy in 10 minutes when dispatched. Dispatched within 10 minutes in response to system contingency events. Must be frequency responsive and be able to run for 2 hours.
10 minutes If generation configured properly, and operating, could be provided in generating mode.
No No
Non-Spinning Reserve
Non-spinning reserve is Off-line Generation Resource capacity
10 minutes If generation configured properly, and
No No
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Market/Service Definition Time Period Applicable to Groundwater Bank Pumped
Storage Facilities
WSWB APH Simulation
WSWB PHPS
Simulation
that can be synchronized to the grid and ramped to a specified load within 10 minutes and run for at least 2 hours.
operating, could be provided in generating mode
Regulation Energy Management (REM)
Regulation energy is used to control system frequency, which must be maintained very narrowly around 60 hertz. Composed of regulation up (increased generation) and regulation down (decreased generation). Capacity that follows (in both the positive and negative direction) a 4-second ISO power signal. It requires 1 -hour of continuous response. Capacity is limited by the resource's 5-minute ramp.
5-10 minute, must be available for 60 minutes
Have to be operating and include equipment necessary to follow regulation signal.
No No
Flexible Ramping
The ability to change generation (ramp) in response to system needs. Requires participation in market with bids and 3-hour continuance response capability.
5 minutes Depends upon pump and generator characteristics
No, response time too slow
Yes
Investment Deferral
The ability to defer additional investment in distribution system, substations, or transmission lines. Resource capable of reliably and consistently reducing net loading on desired infrastructure.
Year Depends upon location of groundwater bank
No. Area of WSWB is an unconstrained SCE area
No. Area of WSWB is an unconstrained SCE area
Reactive Power/Voltage Support
The injection or absorption of reactive power to maintain transmission system
Seconds If generation configured properly
No No
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Market/Service Definition Time Period Applicable to Groundwater Bank Pumped
Storage Facilities
WSWB APH Simulation
WSWB PHPS
Simulation
voltages within required ranges. Resource capable of dynamically correcting excursions outside voltage limits as well as supporting conservation voltage reduction strategies in coordination with utility voltage/reactive power control systems.
Resource Adequacy Capacity (RA)
Assurance that there is adequate physical capacity in existence to serve likely peak load and the ability of the ISO to call on it to perform when needed for system reliability. Must provide net qualifying capacity (NQC) for 4 hours over 3 consecutive days up to a total of 24 hours per month. The resource must bid into the ISO day-ahead and real-time markets.
Hour For flexible capacity, and be 2 hours charging and 2 hours discharging.
No No
Demand Response
Demand response is a change in the power consumption of an electric utility customer in response to utility system needs (typically a reduction in customer demand)
Hour In both generating and pumping mode.
Yes, if additional extraction wells added.
Yes, if additional extraction wells added.
Black Start Generation able to start itself without support from the grid and with sufficient real and reactive capability and control to be useful in system restoration.
Minutes If water stored at elevation, and generation configured appropriately.
No No
Source: (House L. W., 2017 b)
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5.4.2 Statewide Potential from Adding Pumped Storage to Groundwater Banks
Technical feasibility analysis detailed in Chapter 4 indicates that the statewide PHPS potential is
44 MW and statewide demand response potential associated with existing well pumps at
groundwater banks is 220 MW.
Groundwater storage projects can have a variety of configurations, depending upon sources of
water, the configuration of the underground storage basin, method of getting water
underground (either passive via recharge basins that let the water percolate into the ground or,
less frequently, active injection of water into the ground). While all groundwater banks may not
have enough topographical variation to support hydroelectric generation, they all have one
thing in common, an electricity demand when they are extracting the water from underground
for delivery to customers. And, depending upon their delivery requirements, they may have the
ability to vary that pumping load to accommodate electrical system needs.
Table 32 provides an estimate of the statewide potential for pumped storage, hydropower
generation using PHPS facilities, and demand response at groundwater banks. The annual net
benefit, and the expected capital cost was extrapolated from WSWB specific analysis.
Table 32: Statewide Potential, Benefits, and Costs of Pumped Storage at Groundwater Banks
Type MW potential
Annual Net Benefit
Facilities Needed
Capital Cost NPV per kW1
Peak Hour Pumped Storage (PHPS) Facilities – generation, pumped storage
44 MW $-44K2 Upper and lower surface storage reservoirs, connecting piping, hydroelectric generators and controls, utility interconnection
$66.8M ($1,518/kW)3
-$190/kW
Aquifer Pumped Hydro (APH) Facilities –pumped storage
Impractical -$431/kW Surface storage reservoir, reversible pump turbines and controls, connecting piping, utility interconnection
($5,000/kW)4 -$4,945/kW
Flexible Load (Demand Response)
220 MW $6.3M5 Surface storage reservoirs, existing and additional extraction wells
$18M ($82/kW)6
$332/kW
1Assuming a 20-year life and a 6% interest rate. Based upon generating capacity for pumped storage and hydropower
generation, and curtailed capacity for demand response.
2The probability weighted annual net benefit for WSWB PHPS facility generation was -$17/kW.
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3The capital cost of WSWB PHPS facilities was $1,518/kW
4The capital cost of WSWB APH was $5,000/kW.
5The annual net benefit for demand response was $29/kW.
6The capital cost of adding a 5 hours’ surface storage reservoir (to provide 320 hours/year curtailment) and additional
extraction wells was $82/kW (cost for extra wells was $78.1/KW and cost for reservoir was $3.9/kW for a total of $82/kW).
Source: (House L. W., 2017 b)
Demand Response is a very cost effective investment with an annual statewide benefit of $6.3
M. Aquifer Pumped Hydro (APH) never pays for itself, due to high capital cost, low round trip
efficiencies, and limited operating flexibilities. PHPS is cost effective, if operated with dry year
demand response. Assuming statewide PHPS projects have similar characteristics as the WSWB
PHPS facility, the 44 MW PHPS statewide potential (providing pumped storage in neutral years
and hydropower generation in wet years) would have an annual net benefit of $5.9 M if
evaluated with onsite dry year demand response (House L. W., 2017 b).
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CHAPTER 6: Project Benefits
Pumped storage at groundwater banks will provide benefits to the electrical grid. Facilities used
for pumped storage can also be used for hydropower generation and demand response. This
section discusses the benefits associated with each of these operating configurations.
6.1 Addressing the Duck Curve Problem The pumped storage facilities at groundwater banks could assist in addressing “duck curve”
operation issues in all hydrologic years. California is experiencing an abundance of renewable
generation, and this is causing system operating issues. As illustrated in Figure 16, there is a
huge amount of solar generation occurring during the afternoon hours.
Figure 16: Renewable Energy Generation, April 27, 2017
California ISO data for April 27, 2017
Source: (House L. W., 2017 b)
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This overabundance of solar generation during afternoon hours has resulting in the operating
phenomenon known as the “duck curve”, so named by California ISO staff due to its
resemblance to the bird profile (Figure).
The ISO “duck curve” is the net generation load – generation requirements after renewable
generation has been subtracted out. Figure 17 illustrates the operational issues facing
California: specifically, an overabundance of renewable generation during the afternoon hours,
a very steep ramping requirement during the late afternoon, and a peak generation requirement
during the evening. The “duck curve” is forecasted to only get worse as California installs more
and more renewable generation.
Figure 17: California ISO “Duck Curve”
Source: (California ISO; National Renewable Energy Laboratory; First Solar)
A number of methods have been proposed for coping with an increasing “duck curve”,
including:
Exploiting regional diversity in generation resources and demand
Installing more dispatchable generation
Adding more energy storage
Increased demand management:
Time-of-use pricing (TOU) and real-time pricing
Increased demand response
Smart grid technology
85
Onsite pumped storage facilities at WSWB illustrate how these facilities can be employed in
various configurations and hydrologic years to mitigate the duck curve problem. WSWB is an
example of a typical groundwater banking operation and the benefits can be duplicated at other
groundwater banks that have pumped storage potential.
6.1.1 Wet Hydrologic Year
During a wet hydrologic year, the WSWB can operate as a hydroelectric generator. As illustrated
in Figure 18, the Bank’s operations can be configured to curtail generation for 5 hours per day,
ideally during the afternoon renewable generation overproduction period. This would assist
with the “belly” of the “duck curve”, the period of renewable energy overgeneration.
Figure 18: WSWB PHPS Hypothetical Operation During Wet Year
Figure 18 shows WSWB PHPS facility operating as generator
Source: (House L. W., 2017 b)
6.1.2 Neutral Hydrologic Year
During a neutral hydrologic year, the WSWB can operate as a pumped storage facility. Figure
19 show the PHPS operation, from the StorageVet simulation based upon Day Ahead market
prices. PHPS provides generation during the morning and evening ramp periods, and increased
demand (load) during the afternoon renewable overproduction periods to refill storage
reservoirs.
86
Figure 19: WSWB PHPS Hypothetical Operation During Neutral Year
Figure 19 shows WSWB PHPS facility operating as pumped storage
Source: (House L. W., 2017 b)
6.1.3 Dry Hydrologic Year
During a dry hydrologic year, the WSWB operates as a load (pumping water out of the ground
and delivering it to California Aqueduct) and could be configured to accommodate 5 hours of
curtailment if necessary. Figure 20 shows hypothetical WSWB operation during this period,
using the surface reservoirs. WSWB can be configured to reduce load during the late afternoon
ramping period and evening peak.
Figure 20: WSWB Hypothetical Operation During Dry Year
Figure 20 shows demand response operations at WSWB
Source: (House L. W., 2017 b)
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6.2 Greenhouse Gas (GHG) Emissions Reduction Peak Hour Pumped Storage (PHPS) facilities will benefit the environment because they can
potentially be used regardless of the hydrological year type and can reduce the need for fossil
fuel based power plants, thereby resulting in greenhouse gas emissions reduction (Table 33).
Table 33: Annual GHG Emissions Reduction from PHPS at Groundwater Banks
Statewide PHPS
potential at groundwater Banks (MW)
kWh generated by natural gas based
peaker plants
Heat Rate (therm/kWh)
for natural gas fired peaker
plants
kWh generated by pumped storage at
groundwater banks*
Therm reduced
Metric tons of CO2e GHG
reductions**
44 3310*10^6 0.1027 80,300,000 8,250,000 44,000
For Table 33 only Peak Hour Pumped Storage (PHPS) potential was considered since Aquifer Pumped Hydro (APH) is
impractical for large scale deployment.
* Assuming statewide implementation of PHPS for 5 hours daily over 365 days.
**To provide a conservative estimate of GHG Emissions reduction, the analysis has been restricted to an idle or neutral
year when no recharge activities are taking place. The annual GHG reductions will be more in a wet or recharge year since
pumped storage can be supplemented or replaced with hydropower generation that can potentially occur up to 24 hours a
day year-round in a wet year. The GHG reductions may be less in a dry or extraction year depending on how much
capacity is available to implement pumped storage.
Sources:
KWh generated by Peaker Plants (Table 2 page 3 (Nyberg, 2014))
therm/kWh converted from Heat Rate (Btu/kWh) (Table 2 page 3 (Nyberg, 2014))
Emissions Factor(CO2e) for Gas: 0.0053 metric tons/therm (Table 3 (California Energy Commission, 2015 a))
88
CHAPTER 7: Results and Conclusions
Energy storage shifts the renewable energy from the belly (excess) to the head (shortage) of the
‘duck curve’ thereby supplying the electric grid when the generation requirements ramp up and
peak. Pumped storage at groundwater banks has the potential to provide 44 MW of storage
capacity in California. Assuming the State needs 6000 MW of storage to meet the 50% renewable
penetration goal by 2030, implementing pumped storage at groundwater banking projects can
meet up to 1% of the State’s storage needs and provide additional benefits in the form of
demand response and year-round hydropower generation.
The analysis shows that based on the hydrological year type, a typical groundwater banking
operation can use pumped storage facilities to provide hydropower generation and demand
response services besides pumped storage. Additionally, a pumped storage operating
configuration permits participation in multiple markets. Therefore, the Bank operating in the
PHPS mode in a neutral year can participate in flexible ramping and demand response markets
as well as in the Day Ahead Market. It is of interest to note that the traditional way for
evaluating pumped storage – using Day-Ahead energy market prices and generating when
prices are high and extracting water when prices are low, is the least valuable of the services
evaluated. In a dry year, the Bank can participate in the demand response market to provide
various types of demand response. This demand response potential has the greatest value and
configuring the operations to provide demand response in a dry year also enhances the
economic feasibility of pumped storage and hydropower generation operations in neutral and
wet years respectively. Demand response will be online in 1/3 years and incorporating PHPS at
a groundwater banking project can provide revenue during the remaining 2/3 of the years when
Demand response is offline.
The technical, operational and economic analyses show that Aquifer Pumped Hydro (APH)
technology has significant round-trip losses that makes it economically non-viable for most
groundwater banking regions having typical transmissivities. ASR projects that use injection
wells to recharge water may have the potential to generate energy during recharge activities in a
wet year. The decision on installing a generator in an injection well is not clear-cut and will have
to be determined on a case by case basis since the associated capital costs can be prohibitive.
For the agencies that are not already injecting treated recycled water, the increased costs to
treat the water before it can be injected and other regulatory costs make it economically
infeasible to pursue well field generation. Therefore, an APH setup has significant efficiency
constraints that will generally make the technology less viable than PHPS though individual site
characteristics will determine which (if any) technology is more feasible at a particular
groundwater banking site. The APH and PHPS templates developed as part of this study can be
used by existing and planned groundwater banking operations to determine the potential of
either or both pumped storage systems at a particular site. More studies are needed to address
the knowledge gaps related to statewide pumped storage potential at groundwater banks and
89
to move the technology towards implementation. An important next step in this process is a
pilot or field test. The evaluation templates and the groundwater banks database created for
this project provide a good starting point to identify candidate sites for in-depth evaluation and
testing of either or both of the systems.
90
GLOSSARY
Term Definition
ASR (Aquifer Storage
and Recovery) project
A type of groundwater banking project that uses injection wells
to inject water underground for storage when water is available
and later recovers the water from the same well.
cloud data
Cloud data refers to data accessed, managed and transmitted
through the cloud. The cloud refers to a network of servers that
enable a user to access a range of storage and applications
services remotely via the Internet.
CO2e (carbon dioxide
equivalent)
Carbon dioxide equivalent is the standard unit to measure and
compare the emissions from various greenhouse gases based
upon their global warming potential. The global warming
potential of each different greenhouse gas is expressed in terms
of the amount of carbon dioxide that would cause the same
amount of global warming.
demand response
Demand response is the change in electricity consumption in
response to the electric grid needs, electric rates and/or
incentives.
EPIC (Electric Program
Investment Charge)
The Electric Program Investment Charge, created by the
California Public Utilities Commission in December 2011,
supports investments in clean energy technologies that benefit
electricity ratepayers of Pacific Gas and Electric Company,
Southern California Edison Company, and San Diego Gas &
Electric Company.
hydrologic year type
Three hydrologic year types are used in this study: “wet” is the
California Department of Water Resources (DWR) definition of a
wet year; “neutral” is above normal and below nomal year types,
and “dry” is the DWR defined dry and critical hydrologic year
types based on Sacramento River data since 1906 (DWR, 2017).
Supervisory Control
and Data Acquisition
(SCADA)
A system often used in water, energy, and other industries for
controlling equipment operations and gathering real time data
remotely.
T (Transmissivity) Transmissivity is the rate of horizontal flow of groundwater
through an aquifer (underground water-bearing rock or soil).
Water bank or
Groundwater bank
An underground storage facility used for banking or storing
water. Stored water can be recycled, imported or surface water.
91
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A-1
APPENDIX A: Sensitivity Analysis
This document provides an analysis of the parameters that affect the calculation of mounding
losses, which have a direct impact on the potential power generation and provides conclusions
on which parameters have the greater impact on mounding losses relative to others.
Equations Utilized
Power generation potential is calculated utilizing the following procedure:
Step 1 – A theoretical equation will be used to calculate hm = potential mounding (feet) in the
aquifer due to injection of flow through the well into the aquifer. The equation1 in imperial
units is:
hm = ( 2.3 * Q ) x Log (2.25 * T * t)
(4 * 3.14 * T) ( r2 * S )
The equation is the Cooper-Jacob approximation to the Theis equation. The equation provides
the height of injection mound by correlating the drawdown, or head to the negative drawdown
(height of the injection mound).
Q= injection flow rate (ft3 /minute); S = Storage Coefficient; T= Transmissivity of aquifer (ft2
/minute); t = time (minutes); r = well radius (ft.). If hm is known from actual field data, then it
can be used in Step 2 instead of the theoretical value calculated in Step 1.
Step 2 - The hm = potential mounding (feet) calculated in Step 1 will be used to calculate the
available Ht = Head to Turbine for power generation using the equation: Ht= H (depth to water
datum) – hm. Then, P = potential power generation is calculated from the equation below in
imperial units:
P = Q * Ht * E * 0.746 P = kW (kilowatts); Ht = Head on turbine (feet)
3960 Q = Injection flow rate (gallons per minute)
E = turbine efficiency
1 horsepower (hp) = 746 watts = 0.746 kW = 3,960 gpm-ft.
To evaluate the effect of each input parameter in the potential mounding head loss equation =
hm, refer to the attached excel spread sheet. Each of the parameters is varied and the effect on
mounding head loss is evaluated.
A-2
T= Transmissivity; Q= Flow Rate; r = well radius; S = storage coefficient; T = time period
The resulting impacts on hm = mounding head loss is as follows:
Variable Range of hm Overall Effect Specific Impact
T = 3,526 ft.2/day
T = 20,000 ft.2/day
hm = 91.7 ft.
hm = 18.8 ft.
A 467% increase in T,
results in 80%
decrease of hm
For each 6% increase
in T results in 1%
decrease in hm
Q = 1,800 gpm
Q = 2,000 gpm
hm = 16.9 ft.
hm = 18.8 ft.
An 11% increase in Q,
results in 11%
increase in hm for a
given T.
Each 1% increase in Q
results in 1% increase
in hm for a given T.
r = 1.0 ft.
r = 2.0 ft.
hm = 91.7 ft.
hm = 79.7 ft.
A 100% increase in r,
results in 13%
decrease in hm for a
given T.
For each 8% increase
in r results in 1%
decrease in hm for a
given T.
S = 0.001 confined
aquifer
S = 0.1 unconfined
aquifer
hm = 171.1 ft.
hm = 115.5 ft.
A 10,000% increase in
S, results in 33%
decrease in hm for a
given T.
Each 303% increase in
S results in a 1%
decrease in hm for a
given T.
t = 350 minutes
t = 400 minutes
hm = 123.5 ft.
hm = 125.1 ft.
A 14 % increase in t,
results in 1% increase
in hm for a range of T.
Each 14% increase in
t, results in a 1%
increase in hm for a
given T.
Results
Based on the sensitivity analysis Flow Rate, Transmissivity and well radius have the greatest
impact on mounding losses. The lower the injection flow rate and larger the well radius the
lower the resulting hm = mounding losses. With an 11% increase in flow rate from 1,800 gpm to
2,000 gpm the mounding losses increase 11% for a given Transmissivity (this can be expected
by examination of the hm equation). The storage coefficient S is fixed for an unconfined aquifer
such as WSWB, however as the S decreases to a confined aquifer condition where S = 0.001, the
mounding head loss increases by approximately 33% over a range of Transmissivity. As the t =
time increases the mounding losses tend to increase.
Finally, one of the questions that the Technical Advisory Committee (TAC) requested be
considered in the study was, “Does temperature of recharge water have an effect on hydraulic
conductivity of the aquifer materials as it relates to potential power generation with Aquifer
Pumped Hydro (APH) technology?
A-3
UC Berkeley and David Keith Todd Consulting Engineers, Inc. [1] provide the following
definitions:
Given that T= transmissivity = K*t where K= hydraulic conductivity and t= aquifer thickness.
The hydraulic conductivity of a soil is its ability to transmit in a unit of time a unit volume of
groundwater at the prevailing kinematic viscosity of the water through a unit section of area.
Intrinsic permeability is the ability of a soil to transmit a fluid; and is defined by the following
equation:
k = intrinsic permeability = K * u * 1/ (unit weight of water x gravity); where u is the dynamic
viscosity of water. As can be seen in the figure below, dynamic viscosity decreases with
increasing temperature.
If surface water for recharge is colder than 50 to 60 degrees F, the water will warm to the
temperature of groundwater as it percolates into the aquifer. Within the upper 1,000 feet of
soils the groundwater temperature ranges from 50 to 60 degrees F, therefore, very cold
recharge water will have negligible effect on mounding losses
Source: [2]
Reference:
[1] UC Berkeley and David Keith Todd Consulting Engineers, Inc. Groundwater Hydrology,
Second Edition. John Wiley & Sons Publisher.
[2] The Engineering Toolbox. (2017, June 23). Retrieved June 23, 2017, from
http://www.engineeringtoolbox.com/water-dynamic-kinematic-viscosity-d_596.html
B-1
APPENDIX B: Field Measurement of Well Startup & Shutdown Time Durations
Test Protocol
1. Field Ops. Staff (FOP = Steve Tapia) stands at Well K-160.
2. FOP walks to, and enters truck, drives to Well G-160, and stops truck.
3. FOP exists truck, performs start-up on G-160, and signals when flow meter indicates
full flow rate.
4. FOP preforms shut-down of G-160, and signals when well and flow stops.
5. FOP walks to, and enters truck, drives back to Well K-160, and stops truck.
Assumption: 15 MPH Speed Limit (per Berkshire Hathaway Energy’s (BHE's) protocol)
Field Data
Activity Description Duration Seconds (range)
Comments
TRAVEL: Well to well
Field Ops. Staff (FOP) standing at Well K-160 walks to, and enters truck, drives to Well G-160, and stops truck.
118 to 160
Average = 140
Depends on driving speed, distance between wells, and distance truck is parked from a well. (K-160 & G-160 are ½ mile apart.)
BHE’s protocol sets a Speed Limit of 15 MPH.
TURN ON WELL:
FOP exits truck, walks to well head, performs start-up on G-160, and signals when flow meter indicates full flow rate.
18 to 37
Average = 28
Depends on multiple factors:
Distance truck is parked relative to well
Whether well is equipment with “Soft Start” motor control or has the old instant start panels, and also ramping settings of Soft Start Panel.
H.P. of the Well Motor.
Depth of water and size of column pipe.
Flow rates across pump curves.
B-2
Activity Description Duration Seconds (range)
Comments
TURN OFF WELL:
FOP exits truck, walks to well head, turns off well at panel, and signals when motor has come to full stop.
16 to 28
Average = 22
Similar variables to above.
TRAVEL: Well to well
Field Ops. Staff (FOP) standing at Well G-160 walks to, and enters truck, drives to Well K-160, and stops truck.
118 to 160
Average = 140
Depends on driving speed, distance between wells, and distance truck is parked from a well. (K-160 & G-160 are ½ mile apart.)
BHE’s protocol sets a Speed Limit of 15 MPH.
Results:
Start-up duration: 140 [travel] + 28 [turn on well] + 140 [travel] = 308 sec. = 5.13 minutes/well
Shut-down duration: 140 [travel] + 22 [turn well off] + 140 [travel] = 302 sec. = 5.03
minutes/well
It would take one operator over 5 hours to start or stop all 62 wells if they are not equipped
with remote start and stop capability.
C-1
APPENDIX C: WSWB Upper and Lower Reservoir Site Maps
This appendix is available as a separate volume, Publication Number CEC-XXX-2017-XXX-APC
D-1
APPENDIX D: Statewide Survey Results
Statewide Survey Responses
Lead Agency Proceed or
Not with
Pumped
Storage
(Yes/No)
Reason
Central Coast Hydrologic Region
Monterey Peninsula Water
Management District (MPWMD) - ASR
Yes Proceed for Peak Hour Pumped Storage
(PHPS) and Aquifer Pumped Hydro (APH)
studies. They are currently operating an ASR
project and survey indicates pipeline system
does pump recovered water back to source
conveyance in Carmel Valley.
Monterey Regional Water Pollution
Control Agency
No They do not have any service wells nor do
they operate any groundwater bank.
Pajaro Valley Water Management
Agency
No They do not have any ASR project nor
injection wells. There is no indication if pump
water goes back to source conveyance.
Goleta Water District Yes Proceed for Aquifer Pumped Hydro (APH)
study only. They do have an ASR project as
well as injection wells
Santa Barbara, City of, Water
Resources Division
Yes They may have potential for Peak Hour
Pumped Storage (PHPS) technology. There
is significant elevation difference between
source conveyance and recharge facility for
energy generation.
Colorado River Hydrologic Region
D-2
Lead Agency Proceed or
Not with
Pumped
Storage
(Yes/No)
Reason
Coachella Valley Water District
(CVWD)
No They do not have an ASR project or any
injection wells. No indication if water gets
pumped back to source conveyance
Sacramento River Hydrologic
Region
Sacramento Groundwater Authority
(SGA)
No They do not have an ASR project or any
injection wells. They do not manage their
own water directly, but they do oversee their
Joint Powers Authority (JPA)
Sacramento Regional County
Sanitation District (Regional San) The
Nature Conservancy
No They do not have an ASR project or any
injection wells. They also do not manage any
ground water banks.
Sacramento Suburban Water District Yes They may have potential for Aquifer Pumped
Hydro (APH) technology. They do not have
an ASR project, but they do have 88 active
wells and most wells have 200 ft. of ground
water depth or more.
Regional Water Authority No They do not manage any water banks.
Instead, they oversee the operations of other
water agencies.
Yuba County Water Agency No They do not have an ASR project or any
injection wells. They also do not have an
existing pipeline system. They do have a
canal system that is used for in-lieu recharge
only.
City of Tracy - ASR Yes Proceed for Aquifer Pumped Hydro (APH)
study and maybe for Peak Hour Pumped
Storage (PHPS). They have nine extraction
D-3
Lead Agency Proceed or
Not with
Pumped
Storage
(Yes/No)
Reason
wells with one well also used for injections.
They have a pilot ASR project. They do have
an existing pipeline system, not sure
however if water is pumped back to the
source
City of Roseville - ASR No Their water agency currently only uses
surface water, with no water pumping from
wells. They do have ASR wells, but only turn
on ASR wells once a month for testing
purposes.
San Francisco Bay Hydrologic
Region
Zone 7 Water Agency - ASR No They replied via Email that they do not
operate any ground water bank
Santa Clara Valley Water District
(SCVWD) - ASR
No They do not manager their own water
supply. They recommend to contact
Semitropic or Kern County water agencies
for information. They do not have any ASR
or injection wells.
San Joaquin County No They do not manage any ground water
banks currently
San Joaquin River Hydrologic
Region
Stockton East Water District (SEWD) No They may have potential for Aquifer Pumped
Hydro (APH) technology. Their ground water
project site does not have any elevation
difference or existing pipeline system.
D-4
Lead Agency Proceed or
Not with
Pumped
Storage
(Yes/No)
Reason
Instead, the water is transferred through the
use of canals
Northeastern San Joaquin County
Groundwater Banking Authority
No Their Joint Powers Authority (JPA) consists
of 11 members. They oversee other water
agencies and do not manage any ground
water banks directly.
Root Creek Water District Yes They may have potential for Aquifer Pumped
Hydro (APH) technology. They do not have
ASR or injection wells, but they do have 15
wells with at least 350 ft. depth to ground
water level.
South Coast Hydrologic Region
Camp Pendleton - ASR No Their injection wells are used to pump water
for salt water barrier. Their project site is not
a ground water banking site
Compton Water Department Yes Proceed for Aquifer Pumped Hydro (APH)
only. They currently have active ASR project.
Foothill Municipal Water District Yes Proceed for Aquifer Pumped Hydro (APH)
only. They have three injection wells in
service at their project site.
La Verne, City of; Three Valleys
Municipal Water District
City of Lakewood No All the water that flows through their service
area are traveling in one direction and they
do not have any injection wells
D-5
Lead Agency Proceed or
Not with
Pumped
Storage
(Yes/No)
Reason
Orange County Water District Yes Proceed for Aquifer Pumped Hydro (APH)
only. They have 200 large wells in their
service area, and they have injection wells
for basin replenishment.
Los Angeles County Department of
Public Works - ASR
No They do not have any ASR projects or use
any aquifers for storage
Los Angeles Department of Water and
Power - ASR
No They do not have any current ASR projects
or use any aquifers for storage
Main San Gabriel Basin Watermaster No They do not have any ground water banks.
They oversee the operations of other water
agencies.
Cucamonga Valley Water District No They do not have any injection wells. The
water flows through their service area in one
direction only.
Eastern Municipal Water District - ASR No They do not have any injection wells. The
water flows through their service area in one
direction only.
Raymond Basin Management Board -
ASR
No They are a Watermaster that oversee other
water agencies, they do no manage any
ground water projects. Their water operating
system does not have elevation difference or
put/take amounts.
San Bernardino Valley Water
Conservation District
No They do not have an existing pipeline
system, ASR project, or extraction wells
Three Valleys Municipal Water District No They already have a hydroelectric facility.
They do not have any injection wells
D-6
Lead Agency Proceed or
Not with
Pumped
Storage
(Yes/No)
Reason
Helix Water District [El Monte Valley] No They do not have an ASR project or any
injection wells. They also do not manage any
ground water facilities
Sweetwater Authority No They do not have any ASR project or
manage any ground water banks. They have
a desalination plant that utilizes reverse
osmosis to purify water for customer use
United Water Conservation District -
ASR
No Their project site has low elevation
difference, and no existing pipeline system.
They do not have any injection wells or ASR
projects
Western Municipal Water District No They do not have any injection wells, nor do
they have an existing pipeline system in
operation.
Castaic Lake Water Agency No Taken from survey response: Castaic Lake
Water Agency (CLWA) does not operate any
ground water banking programs.
South Lahontan Hydrologic Region
Mojave Water Agency Yes They do not have any injection wells. They
may have potential for Peak Hour Pumped
Storage (PHPS) because they have an
existing pipeline system that is in use.
D-7
Lead Agency Proceed or
Not with
Pumped
Storage
(Yes/No)
Reason
Tulare Lake Hydrologic Region
Kern Water Bank Authority No The elevation difference at their project site
is not enough for Peak Hour Pumped
Storage (PHPS) technology. They do not
have any injection wells.
City of Bakersfield 2800 Acre Water
Bank
Yes They do not have an ASR project, but they
have 53 wells with deep enough 340 ft.
depth to groundwater level
James Irrigation District No Prior research found their project site to have
low elevation difference, and no existing
pipeline; Background study also found
injection wells inefficient
Rosedale-Rio Bravo WSD
Wheeler Ridge Maricopa Water
Storage District
No They do not have any pumped storage or
aquifer storage facilities
Shafter Wasco Irrigation District No They are just getting started on building out
their ground water bank facility and wells.
They are not in operation yet.
Southern San Joaquin Municipal
Utilities District
No They are trying to outsource their water.
They do not operate any ground water banks
currently
Kaweah Delta Water Conservation
District
No They do not have any pump storage in
operation
Pixley Irrigation District/Lower Tule
River Irrigation District
No They only have surface water storage for
agriculture, but no pipeline system available
D-8
Lead Agency Proceed or
Not with
Pumped
Storage
(Yes/No)
Reason
North Coast Hydrologic Region
Butte County No They do not manage or own any water
banks
E-1
APPENDIX E: Small Hydropower Potential for Groundwater Banking Agencies
Geographic Region
Hydrologic Region
County Total Annual Water
Entitlements (AWE) for
County (AFY)
Water Purveyors having
Groundwater Banking Projects a
Annual Water Entitlements
(AWE) for Water
Purveyor (AFY)b
Countywide Small
Hydropower Potential
(kW)c
Estimated Small
Hydropower Potential (kW) for Water
Purveyors N San
Francisco Bay
Alameda
260,000
Alameda County Water District
(ACWD)
42,000
3,200 3,200
East Bay Municipal Utilities District
(EBMUD)
150,000
Alameda County FC & WCD, Zone 7
68,000
3 260,000C Tulare Lake Fresno
2,446,395
City of Fresno 60,000
6,426 2,503
Consolidated Irrigation District
(CID)
240,000
Fresno Irrigation District (FID)
550,000
James Irrigation District
59,220
Tranquillity Water District/Tranquillity Irrigation District
43,857
E-2
Geographic Region
Hydrologic Region
County Total Annual Water
Entitlements (AWE) for
County (AFY)
Water Purveyors having
Groundwater Banking Projects a
Annual Water Entitlements
(AWE) for Water
Purveyor (AFY)b
Countywide Small
Hydropower Potential
(kW)c
Estimated Small
Hydropower Potential (kW) for Water
Purveyors
5
953,077 S South
Lahontan Kern
2,461,275
Antelope Valley Water Storage
250000d 19,177 21,860
Tulare Lake Arvin-Edison Water Storage District
(AEWSD)
351,675
Berrenda Mesa Water District
(BMWD)
140,000
Buena Vista Water Storage District
(BVWSD)
185,000
Cawelo Water District
75,000
Kern Delta Water District
220,000
Kern Tulare Water District
40,000
North Kern Water Storage District
222,000
Rosedale-Rio Bravo WSD (RRBWSD)
70,000
Semitropic Water Storage District
500,000
Shafter-Wasco Irrigation District
(SWID)
89,600
Tehachapi-Cummings County
Water District (TCCWD)
25,000
E-3
Geographic Region
Hydrologic Region
County Total Annual Water
Entitlements (AWE) for
County (AFY)
Water Purveyors having
Groundwater Banking Projects a
Annual Water Entitlements
(AWE) for Water
Purveyor (AFY)b
Countywide Small
Hydropower Potential
(kW)c
Estimated Small
Hydropower Potential (kW) for Water
Purveyors Wheeler Ridge Maricopa Water Storage District
(WRMWSD)
220,000
13
2,138,275 C Tulare Lake
Kings
582,508
Kings County Water District Apex Ranch
Conjunctive Use (KCWD)
256,938
4,054 1,788
1
256,938 S South
Lahontan Los Angeles
3,807,645
Antelope Valley-East Kern Water Agency (AVEK)
141,000
56,932 20,525
South Coast Los Angeles Department of
Water and Power (LADWP)
795,454
City of Long Beach Water Department
46,475
San Gabriel Valley Municipal Water
Districte
28,800
Three Valleys Municipal Water
District (TVMWD)
51,000
West Basin Municipal Water
District (WBMWD)
160,000
E-4
Geographic Region
Hydrologic Region
County Total Annual Water
Entitlements (AWE) for
County (AFY)
Water Purveyors having
Groundwater Banking Projects a
Annual Water Entitlements
(AWE) for Water
Purveyor (AFY)b
Countywide Small
Hydropower Potential
(kW)c
Estimated Small
Hydropower Potential (kW) for Water
Purveyors Water
Replenishment District of Southern California (WRD) (previously called Central and West
Basin Water Replenishment
District)
150,000
7
1,372,729 C San Joaquin
River
Madera
884,000
Chowchilla Water District
239,000
6,793 4,103
Madera Irrigation District (MID)
295,000
2
534,000 S South Coast
Orange County
318,500
Orange County Water District
(OCWD)
225,000
1,189 840
1
225,000 N Sacramento
River
Placer
231,200
City of Roseville Water District
32,000
778 108
1
32,000 S Colorado
River Riverside
1,123,216
Coachella Valley Water District
(CVWD)
508,100
3,961 2,480
Desert Water Agencyf
38,100
E-5
Geographic Region
Hydrologic Region
County Total Annual Water
Entitlements (AWE) for
County (AFY)
Water Purveyors having
Groundwater Banking Projects a
Annual Water Entitlements
(AWE) for Water
Purveyor (AFY)b
Countywide Small
Hydropower Potential
(kW)c
Estimated Small
Hydropower Potential (kW) for Water
Purveyors South Coast
Eastern Municipal Water District
(EMWD)
77,016
Rancho California Water District
(RCWD)
30,000
Western Municipal Water District
(WMWD)
50,000
5
703,216 S South Coast San
Bernardino
283,417
lnland Empire Utilities Agency
(previously known as Chino Basin Municipal Water
District)
25,000
17,728 12,723
San Bernardino Valley Municipal
Water District (SBVMWD)
102,600
South Lahontan
Mojave Water Agency (MWA)
75,800
3
203,400 N Sacramento
River
Sacramento
196,000
City of Sacramento, Utilities
Departmentg
90,000
1,506 692
1
90,000
S South Coast
San Diego
City of San Diego Public Utilities Department
235,245
4,874 2,254
E-6
Geographic Region
Hydrologic Region
County Total Annual Water
Entitlements (AWE) for
County (AFY)
Water Purveyors having
Groundwater Banking Projects a
Annual Water Entitlements
(AWE) for Water
Purveyor (AFY)b
Countywide Small
Hydropower Potential
(kW)c
Estimated Small
Hydropower Potential (kW) for Water
Purveyors Helix Water District
35,500 Sweetwater
Authority
22,500
634,245 3
293,245 N San Joaquin
River San Joaquin
952,713
Stockton East Water District
(SEWD)
75,000
7,406 1,726
Tulare Lake
Southern San Joaquin Municipal
Utilities District (SSJMUD)
147,000
2
222,000 C San
Francisco Bay
Santa Clara
296,541
Santa Clara Valley Water District
(SCVWD)
252,500
2,058 1,752
1
252,500 C Tulare Lake Tulare
Delano-Earlimart Irrigation District
(DEID)
183,300
12,258 8,559
Kaweah Delta Water Conservation District (KDWCD)
440,000
Lower Tule River Irrigation District
(LTRID)
330,302
Pixley Irrigation District
31,102
Porterville Irrigation Districts
46,000
E-7
Geographic Region
Hydrologic Region
County Total Annual Water
Entitlements (AWE) for
County (AFY)
Water Purveyors having
Groundwater Banking Projects a
Annual Water Entitlements
(AWE) for Water
Purveyor (AFY)b
Countywide Small
Hydropower Potential
(kW)c
Estimated Small
Hydropower Potential (kW) for Water
Purveyors
1,595,072
Saucelito Irrigation District
54,000
Terra Bella Irrigation District
29,000
7
1,113,704
S South Coast
Ventura
115,000
Calleguas Municipal Water District
95,000
154 127
1
95,000 N Sacramento
River
Yuba County
321,000
Yuba County Water Agency (YCWA)
300,000
2,464 2,303
1
300,000
Notes
a The listed water purveyors have groundwater banking projects as identified in the master database, "CA Groundwater Banking Projects" compiled for this study. Where
more than one water purveyor is listed for a water entitlement, at least one of the agencies has groundwater banking operations. It is assumed that the reference study
(Statewide Small Hydropower Resource Assessment, Navigant Consulting, Inc.) includes all the groundwater banking agencies/districts which have PHPS potential.
b Peak Hour Pumped Storage (PHPS) can happen every year regardless of hydrology and as long as there is available water for 'cycling' an agency should be able to
implement PHPS regardless of source of water. An agency can potentially use water entitlements besides banked water if needed. The water entitlements database was
assembled from multiple sources which include information on water rights, State Water Project (SWP) deliveries, Central Valley Project (CVP) deliveries and well data
(Navigant Consulting, June 2006).
c Small hydropower capacity is defined as 30 MW or less and the minimum size unit to be considered in the source study was 100kW. Very small water purveyors with
annual water entitlements less than 20,000 AFY were not included in the small hydropower (kW) computation since they did not have sufficient amount of water to meet
the source study's (Navigant Consulting, June 2006) minimum threshold of 100 kilowatts generation potential. The remaining Large, Medium or Small agencies total 164 in
number. The source study used estimation factors to calculate kW potential for medium and small purveyors that were not surveyed; the large ones were evaluated
through site survey or interview only and their potential was not used to develop estimation factors (Navigant Consulting, June 2006).
E-8
d Antelope Valley Water Storage (AVWS) was not one of the entities included in the reference database. The peak hour generation potential (via Peak Hour Pumped
Storage) and hydropower generation potential for AVWS (5.2 MW) was calculated as part of this project and has been added to the interpolated small hydropower
potential (kW) for groundwater banking agencies in Kern County.
e Main San Gabriel Basin Watermaster is included in the master database, "CA Groundwater Banking Projects." The Watermaster administers adjudicated water rights
and manages and protects groundwater resources within the Main San Gabriel Groundwater Basin. San Gabriel Valley Municipal Water District is one of the three
agencies delivering supplemental SWP water to the basin for recharge.
f Desert Water Agency and Coachella Valley Water District partner to recharge groundwater (Master Database, CA Groundwater Banking Projects)
g City of Sacramento is a member agency of Sacramento Groundwater Authority. The Authority is included in the master database, "List of CA Groundwater Banking
Projects." The City has participated in water transfer efforts previously and may do so in future (City of Sacramento Department of Utilities. 2010 Urban Water
Management Plan. October 2011. Prepared by Carollo Engineers, Inc.)
Sources:
Small hydropower potential (kW) by County (California RPS-Eligible Small Hydropower Potential (2004 Draft Report), Navigant Consulting, Inc.; California Small Hydropower and Ocean Wave Energy Resources (Staff Paper) (Kane, 2005)
Information about water entitlements for County/Region (Navigant Consulting, June 2006)
Groundwater banking agencies (including those with ASR projects). (Master Database, CA Groundwater Banking Projects. Groundwater Bank Energy Storage Systems: A Feasibility Study for Willow Springs Water Bank. 2017. Prepared by Antelope Valley Water Storage (AVWS), LLC
F-1
APPENDIX F: Well Pumps Demand Response Potential for Selected Groundwater Banking Projects
Hydrologic Region
Lead agency for Groundwater
Banking Project
Groundwater Basin/Subbasin
Name
Recovery (AFY)
Energy Intensity
(kWh/AF)17
Annual kWh
Estimated Pumping Capacity
(kW)18
Notes from literature research/survey
CC Monterey Peninsula Water Management District
Carmel Valley, Seaside
3000 388 1,164,000 199 Phase 1 ASR includes two ASR wells with combined injection capacity 3,000 gpm and recovery capacity 3,500 gpm. Phase 2 ASR project includes two ASR wells with maximum annual diversion limit of 2,900 acre-feet/year, combined injection rate of 3,600 gpm, and annual yield of 1,000 acre-feet.
SC Elsinore Valley Municipal Water District; Western Municipal Water District
Elsinore Valley, Riverside-Arlington and Temescal
4000 541 2,164,000 370
SC Foothill Municipal Water District
- 3000 541 1,623,000 277
SC Inland Empire Utilities Agency
- 140,000 541 75,740,000 12934
17 Energy Intensity is for the year 2000, a "normal" water year from Table G-1 in Embedded Energy in Water Studies Study 1: Statewide and Regional Water-Energy Relationship (GEI Consultants/Navigant Consulting, Inc., 2010)
18 To calculate annual kW demand, around-the-clock operations for 244 days (~ 8 months) are assumed regardless of whether a project is in-lieu or has direct artificial recharge. It is assumed that the recovery operations use only electric motors and no diesel engines.
F-2
Hydrologic Region
Lead agency for Groundwater
Banking Project
Groundwater Basin/Subbasin
Name
Recovery (AFY)
Energy Intensity
(kWh/AF)17
Annual kWh
Estimated Pumping Capacity
(kW)18
Notes from literature research/survey
SC Inland Empire Utilities Agency; Three Valleys MWD; Chino Basin Watermaster
Chino, Cucamonga
33000 541 17,853,000 3049
SC La Verne, City of; Three Valleys Municipal Water District
- 1000 541 541,000 92
SC Long Beach Water Department
Central 4300 541 2,326,300 397
SC Long Beach Water Department and City of Lakewood
Central 1200 541 649,200 111
SC Main San Gabriel Basin Watermaster
San Gabriel Valley
60000 541 32,460,000 5543
SC Orange County Water District
Coastal Plain of Orange County
22000 541 11,902,000 2032
SC San Bernardino Valley Municipal Water District (Valley District)
Rialto-Colton, Bunker Hill, Yucaipa
29500 541 15,959,500 2725
SC San Diego, City of, Public Utilities Department
San Pasqual Valley, San Diego River Valley
5800 541 3,137,800 536
SC Three Valleys Municipal Water District
- 5,000 541 2,705,000 462 There are two groundwater production wells.
SC Water Replenishment District of
West Coast, Central
245000 541 132,545,000 22634
F-3
Hydrologic Region
Lead agency for Groundwater
Banking Project
Groundwater Basin/Subbasin
Name
Recovery (AFY)
Energy Intensity
(kWh/AF)17
Annual kWh
Estimated Pumping Capacity
(kW)18
Notes from literature research/survey
Southern California
SC United Water Conservation District
Oxnard 15000 541 8,115,000 1386 United Water’s Oxnard-Hueneme Delivery System (O-H system) supplies 15,000 AF/year water to several agencies. O-H system is supplied by 12 wells that draw from Oxnard Plain Groundwater Basin. Wells have flow rate 1,800-2,500 gpm, and water to wire efficiencies >65%.
SF Santa Clara Valley Water District (SCVWD)
Santa Clara, Llagas Area
35000 342 11,970,000 2044
SJ Madera Ranch Water Bank, operated by Madera Irrigation District
- 55000 223 12,265,000 2094
SJ Root Creek Water District
Madera 6000 223 1,338,000 228 A total of 15 deep and shallow extraction wells are located across district. Well capacity ranges from 1600 gpm-2000 gpm. This was excluded from further consideration since wells are owned by private land owners which would make demand response program difficult to implement.
F-4
Hydrologic Region
Lead agency for Groundwater
Banking Project
Groundwater Basin/Subbasin
Name
Recovery (AFY)
Energy Intensity
(kWh/AF)17
Annual kWh
Estimated Pumping Capacity
(kW)18
Notes from literature research/survey
SL Willow Springs Water Bank
Antelope Valley 225000 342 76,950,000 13140 The demand response potential at Willow Springs Water Bank is estimated to be 14.0 MW (Details are provided in Chapter 2 of this study). 62 production wells are planned for WSWB. Each production well is expected to have a 300-horsepower motor, or 0.225 MW.
SL AVEK Godde Bank operated by Antelope Valley-East Kern Water Agency
Antelope Valley 40000 342 13,680,000 2336
SL Planned Enterprise Bank operated by Antelope Valley-East Kern Water Agency
Antelope Valley 83300 342 28,488,600 4865
SL Mojave Water Agency
Cronise Valley, Lower Mojave River Valley, Middle Mojave River Valley, Upper Mojave River Valley, El Mirage Valley, Kane Wash Area, Lucerne Valley, Langford Well Lake, Fremont Valley, Goldstone
50000 342 17,100,000 2920
F-5
Hydrologic Region
Lead agency for Groundwater
Banking Project
Groundwater Basin/Subbasin
Name
Recovery (AFY)
Energy Intensity
(kWh/AF)17
Annual kWh
Estimated Pumping Capacity
(kW)18
Notes from literature research/survey
Valley, Superior Valley, Searles Valley, Salt Wells Valley, Grass Valley, Warren Valley, Deadman Lake, Bessemer Valley, Ames Valley, Means Valley, Upper Johnson Valley, Iron Ridge Area, Lost Horse Valley
SL Palmdale Regional Groundwater Recharge and Recovery Project
- 24250 342 8,293,500 1416
SR Sacramento Suburban Water District
- 4500 184 828,000 141 The District provides water to its customers from 88 active groundwater wells. The groundwater basin underlying the District is located in a portion of the North American subbasin: 47 wells with capacity of 180-3500 gpm and 50-250 hp motor, 37 wells (with capacity of 600-2950 gpm and 75-300 hp motor and 3 wells with capacity of 400-650 gpm and 75 hp motor.
F-6
Hydrologic Region
Lead agency for Groundwater
Banking Project
Groundwater Basin/Subbasin
Name
Recovery (AFY)
Energy Intensity
(kWh/AF)17
Annual kWh
Estimated Pumping Capacity
(kW)18
Notes from literature research/survey
SR Yuba County Water Agency
- 30000 184 5,520,000 943
SR Sacramento Regional County Sanitation District (Regional San)/The Nature Conservancy
- 30000 184 5,520,000 943
TL Buena Vista Water Storage District
Kern County 40000 369 14,760,000 2520
TL Semitropic Water Storage District
Kern County 365000 369 134,685,000 22999
TL Arvin-Edison Water Storage District
Kern County 170235 369 62,816,715 10727
TL Kern Water Bank Authority
Kern County 240000 369 88,560,000 15123 Kern Water Bank has no injection wells. Recharge is via approximately 7,000 acres of recharge ponds or in-lieu. There are 85 recovery wells which on average are about 750-feet deep and produce as much as 5,000 gallons-per-minute of water. Wells are spaced 1/3 of a mile or more apart.
TL Fresno Irrigation District (Waldron Pond)
- 9000 369 3,321,000 567
TL North Kern Water Storage District
Kern County 250000 369 92,250,000 15753 The District successfully curtail 9 MW of peak load
F-7
Hydrologic Region
Lead agency for Groundwater
Banking Project
Groundwater Basin/Subbasin
Name
Recovery (AFY)
Energy Intensity
(kWh/AF)17
Annual kWh
Estimated Pumping Capacity
(kW)18
Notes from literature research/survey
using regulating reservoirs, telemetry equipment and timers on over 60 groundwater wells (Burt, Howes, & Wilson, 2003)
TL City of Bakersfield 2800 Acre Water Bank
- 89000 369 32,841,000 5608 The City pumps groundwater from Kern County groundwater basin with 53 active wells. These wells have a combined capacity of about 89,000 AF/year. From survey response, active wells have a flow capacity of 3200 gpm, 250 hp motor, and 40-65% efficiency. (For the calculations of demand response potential, the earlier recovery estimate of 46000 AFY from Pacific Institute Report was replaced by 89000 AFY).
TL Consolidated Irrigation District
- 8000 369 2,952,000 504
TL Kings County WD Apex Conjunctive Use
- 4000 369 1,476,000 252
TL James ID Lateral K
- 2000 369 738,000 126
TL Kern County Water Agency
- 98000 369 36,162,000 6175
TL Rosedale-Rio Bravo WSD
- 62500 369 23,062,500 3938
F-8
Hydrologic Region
Lead agency for Groundwater
Banking Project
Groundwater Basin/Subbasin
Name
Recovery (AFY)
Energy Intensity
(kWh/AF)17
Annual kWh
Estimated Pumping Capacity
(kW)18
Notes from literature research/survey
TL Cawelo Water District
Kern County 5500 369 2,029,500 347
TL Kern Delta Water District
- 94000 369 34,686,000 5923
TL Pixley Irrigation District
Tule 30000 369 11,070,000 1890
TL Wheeler Ridge Maricopa Water Storage District
- 50000 369 18,450,000 3151
TL Buena Vista Water Storage District and West Kern Water District
- 45000 369 16,605,000 2836
TL Kern Co Water Agency Pioneer Recharge and Recovery Project
- 98000 369 36,162,000 6175
TL James Irrigation District
Kings 4000 369 1,476,000 252 Groundwater supply is pumped from 63 extraction wells, 28 wells are within district boundaries, and 35 wells are in easement area of City of San Joaquin. The 63 wells have flow capacity of 2400 gpm, pumping capacity of 210 cfs, and 75% efficiency. It is not clear how many of these extraction wells are used for recovery from groundwater banking project.
TL Berrenda Mesa Water District
- 50000 369 18,450,000 3151
F-9
Hydrologic Region
Lead agency for Groundwater
Banking Project
Groundwater Basin/Subbasin
Name
Recovery (AFY)
Energy Intensity
(kWh/AF)17
Annual kWh
Estimated Pumping Capacity
(kW)18
Notes from literature research/survey
TL Kaweah Delta Water Conservation District
Kaweah 35000 369 12,915,000 2205
TL West Kern Water District
Kern County 20000 369 7,380,000 1260
CR Cadiz, Inc. - 50000 369 18,450,000 3151CR Coachella Valley
Water District Indio, Mission Creek, Desert Hot Springs
300000 369 110,700,000 18904 More than 100 wells across district boundaries pump groundwater.
Total 217354
CC=Central Coast, SC=South Coast, SF=San Francisco Bay, SJ=San Joaquin River, SL=South Lahontan, SR=Sacramento River, TL=Tulare
Lake, CR=Colorado River
G-1
APPENDIX G: List of Required Permits and Registrations
Note- not all of these may be applicable to all groundwater banking sites used for energy
storage.
Agency Permit / Registration
Criteria Comments
FERC – Federal Energy Regulatory Commission
Hydro exemption or license
Will need either a conduit exemption, a 10-MW exemption, or a license, depending upon characteristics of hydro generator
Consult FERC small hydro website: https://www.ferc.gov/industries/hydropower/gen-info/licensing/small-low-impact.asp
Qualifying Facility 80 MW or less using renewable generation
Form 556
EIA - Energy Information Administration
Generator Registration
1 MW or larger EIA Form 860
CAISO – California Independent System Operator
FNM – Full Network Model
1 MW or larger GRDT – Generation Resource Data Template
Interconnection If connected to transmission system
FERC wholesale interconnection application http://www.caiso.com/planning/Pages/GeneratorInterconnection/InterconnectionRequest/Default.aspx
NRI – New Resource Integration
1 MW or larger (occasionally 500 KW or larger)
http://www.caiso.com/Documents/NewResourceImplementationGuide.doc
CEC – California Energy Commission
Small Hydro Certification
Required for RPS (Renewable Portfolio Standard)
CEC RPS-1
Generating Unit ID 1 MW or larger CEC-1304 WREGIS – Western Renewable Energy Generation Information System
QRE (Qualified Reporting Entity) Generating Unit ID
Credit for RECs (Renewable Energy Certificates)
SWRCB – State Water
Nonconsumptive Water Use Right
G-2
Agency Permit / Registration
Criteria Comments
Resources Control Board 401 permit Water Quality
Certification
Electric Utility Interconnection If connected to Distribution System
PPA (Power Purchase Agreement)
If selling output to utility
Environmental Documents
CEQA (California Environmental Quality Act)
EIR (Environmental Impact Report)
USACE (U S Army Corps of Engineers) 404 permit
Discharge permit
CDFW (California Department Fish and Wildlife) 1602 permit
Streambed alteration permit
Source: (House L. W., 2017 b)
I
ATTACHMENT I: Willow Springs Water Bank (WSWB) Fact Sheet
This attachment is available as a separate volume, Publication Number CEC-XXX-2017-XXX-ATI
WILLOW SPRINGS WATER BANK CONJUNCTIVE USE PROJECT ELIGIBILITY A6 – OTHER APPENDIX
Appendix B
ATTACHMENT 2
Executive Summary Form
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1. Project description for “Water/Energy Bank Proof-of-Concept”
The water/energy bank will provide energy benefits by shifting when imported water is delivered to Southern California. The shift utilizes the existing State Water Project (SWP) infrastructure as well as existing and planned groundwater storage facilities. The water/energy bank enables a load shift out of the peak summer period and into the fall, winter and spring months. There is no net increase in energy use, only a shift in its timing. This shift of imported water deliveries uses water storage as a surrogate for energy storage. Existing water storage will be drawn down in the summer. Replacement storage will be provided from groundwater storage facilities such as Willow Springs Water Bank (WSWB). Renewables penetration will increase due to the load shift to a period of over-supply. Unlike other types of storage, this project provides a seasonal load shift that is crucial to reduce solar curtailment in the Spring and peak loads in the Summer. The water/energy bank also enables emergency demand response in the event of a grid emergency. Most or all of the SWP pumping units that convey water over the Tehachapis could be shut down for the duration of the emergency. Water supply would be maintained by drawing down storage. This improves renewables penetration by providing firm load shedding to complement non-firm renewables. The project would develop demand response and load shifting tools and strategies to minimize peak demand and reduce energy costs. It will convert hydrokinetic energy in existing water conveyance and pumps into hydrostatic (potential) energy through water storage. This will enable load shift in response to demand response and price signals. The project aims to shift up to 100% of the peak hour demand in the summer months. Therefore, the project is an excellent fit for GFO-16-305 Group 2.
2. Project goals and objectives
Goals: what this project will achieve Benefit IOU ratepayers: greater reliability, lower cost, and increased safety Overcome barriers to achievement of the state’s energy goals Increase market penetration of distributed renewable generation
Objectives: how the goals will be met - Peak Load Reduction Reduce the amount of SWP water delivered during the peak summer months (wet, normal or dry water years) to shift the electric load used for pumping. It addresses the issue of how to meet peak summer loads with an increasing proportion of renewable energy. - Avoided Renewable Curtailment Shift the pumping for water deliveries into the fall, winter and spring months when over-supply of renewable energy is expected. This will absorb surplus renewables and reduces the risk of over-generation. - Load Following and Ramping for Renewable Integration Provide reliable and predictable load following and ramping that can be timed to reduce morning and evening ramping requirements and reduce the amount of flexible natural gas generation that must be online and at minimum load during the day (increasing curtailment of solar generation). - Emergency Demand Response Use the energy embedded in stored water to provide firm load reduction in the event of a grid emergency.
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Executive Summary Form
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- Onsite Renewable Energy Develop onsite renewable energy to make replacement groundwater storage energy-neutral and equivalent in reliability to existing surface water storage.
3. Explanation of how project goals and objectives will be achieved, quantified, and measured: Project goals and objectives will be achieved by using groundwater storage to shift the timing of when water is pumped to Southern California. Water agencies that currently recharge most of their SWP deliveries will be incentivized to recharge only during the fall, winter, and spring months. Large surface water reservoirs would be provided replacement storage from WSWB. Replacement storage must provide equivalent or better water reliability and cost. Energy shifted can be quantified by measuring the amount of water deliveries shifted. Water pumped over the Tehachapis has 3.2 MWh/acre-foot embedded in it. For example, 54,000 acre-foot shift to the fall, winter or spring months is a 173,000 MWh in energy use out of the summer window. A shutdown of some SWP pumping units that convey water over the Tehachapis would be firm load shedding in the event of a grid emergency.
4. Project task description: The project goals and objectives will be achieved through 6 major tasks: (1) Contractor Outreach: meet with SWP contractors and determine what incentives they
need to shift their delivery schedules. The needs of the contractors who primarily recharge imported water will be different from the needs of contractors and water agencies that have existing surface storage reservoirs for imported water storage.
(2) DWR Operations: coordinate with DWR to determine the extent to which a shift in the SWP delivery schedule can enhance current operations of DWR’s Valley String Pumping Plants and reduce transportation costs via lower electric rates. Also, assess the potential to leverage the energy benefits by adjusting when deliveries are shifted.
(3) Reservoir Operations: assess what is needed to make storage in a groundwater bank equivalently reliable when compared to surface water storage. Also assess the low point mitigation benefits from leaving more water in San Luis Reservoir for storage during the summer months and replacing it during the other months.
(4) Electric Grid: the benefits of a guaranteed imported water delivery shift accrue to the electric grid. IOUs can use this to avoid building new combustion turbines and batteries. An institutional structure needs to be developed to link all of the participants and provide the incentives needed to shift imported water deliveries.
(5) Economics: quantify the economic benefits of reduced peak summer electric load and increased load during periods of expected surplus, including the avoided cost of facilities needed to meet summer peaks, the reduction in the SWP transportation charges, and the increased penetration of renewable energy.
(6) Onsite Renewables Generation: assess how much additional renewable energy can be added at the water/energy bank site to supplement the existing solar arrays.
5. Agreement management description:
Antelope Valley Water Storage (AVWS) has an existing contract with the CEC to study the benefits of pumped storage at a groundwater bank. Consequently, we are familiar with the CEC agreement requirements and project tracking needs. A similar management team and agreement approach will be implemented for this project to ensure on-time and on-budget delivery of the project, with AVWS as the single point of contact.
ATTACHMENT 3 Fact Sheet Template
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Water/Energy Bank Proof-of-Concept
Use of water storage to shift when imported water is pumped to Southern California to provide electric demand response and load shifting
The Issue The State Water Project (SWP) is California’s largest user of electricity. Pumping imported water over the Tehachapi Mountains involves a 2,882’ lift at the four Valley String Pumping Plants and requires up to 1,000 MW of electrical power (about 2% of the state’s anticipated 2020 peak need). Currently, imported water deliveries occur at a relatively constant rate each month. Water storage can be used to shift deliveries from periods of electric shortage in the summer to periods of surplus in the fall, winter and spring. This reduces peak energy needs and increases the penetration of renewable energy. It also provides emergency load reduction if needed.
Project Description The California Department of Water Resources (DWR) already starts and stops SWP pumps daily to optimize electricity use. The monthly delivery schedule, however, is largely determined by the SWP contractors. The contractors focus on making water reliable. The innovation of this project is that contractors will be incentivized to adjust their delivery schedules to optimize energy benefits. This will enable a guaranteed load reduction. The project has the potential to shift up to 100% of the peak hour demand in the summer months. “Green” groundwater storage will be used as replacement storage to enable the delivery shift and reduce peak load. Willow Springs Water Bank (WSWB) can provide replacement storage at equivalent reliability and cost. This novel concept of a water/energy bank also reduces the risk of blackouts by providing emergency demand response and uses dual purpose facilities to generate renewables onsite. Anticipated Benefits for California General benefits: A primary benefit is the reduction of peak summer electricity demand without using fossil fuel combustion turbines or limited-duration batteries. An additional benefit is the ability to increase electricity use during periods of anticipated over-supply of renewable energy. The project also provides emergency demand response and renewable energy onsite.
Specific Benefits
Lower costs The cost to meet peak electricity needs using new combustion turbines or batteries will be avoided with summer reductions of SWP pumping. DWR’s transportation costs to import water will also be reduced by using the lower rates for electricity available during non-summer months.
Greater reliability Improved reliability for the electric grid results from a guaranteed summer pumping
Edmonston Pumping Plant is the largest single user of electricity in California, with each of the 14 pumps using 60 MW of electricity. Image Credit: Pumps & Systems
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reduction that provides firm demand response to match the evening ramp up as solar arrays go offline. It is independent of natural gas availability and can provide peak power for longer durations than batteries. It also provides rapid and dispatchable demand response that can address a grid emergency such as the loss of generation or transmission facilities to improve reliability.
Increased safety Increased safety results from having a source of load reduction in the summer that does not involve natural gas combustion turbines and is not subject to safety issues like the natural gas leak at Aliso Canyon and the explosion at San Bruno.
Economic development Use of existing water infrastructure to meet energy needs reduces the cost and time of implementation. It also reduces the need to purchase energy from investor-owned utilities or sources outside of California during the summer months. Additionally, increased penetration of renewable energy will provide more renewable energy jobs in California.
Environmental benefits Increased penetration of renewable energy and less use of combustion turbines to meet summer peaks reduces greenhouse gas creation. It also decreases California’s dependence on fossil fuels. Replacement storage would be provided from environmentally-friendly groundwater storage, which also provides a site for additional renewable energy.
Public health Leaving water in storage in San Luis Reservoir during the summer months mitigates algae problems that occur during periods when the volume of water in the reservoir drops below 300,000 acre-feet. Algae blooms cause taste and odor problems and may involve toxic blue-green algae.
Consumer appeal Using existing infrastructure better avoids the construction of new dams or new diversions from waterways, reduces reliance on natural gas, and avoids the construction of new combustion turbines. This should appeal to consumers. It also reduces the chances of electrical outages by providing dispatchable demand response.
Energy security Increased use and penetration of renewable energy during periods of anticipated over-supply and over-generation reduces California’s dependence on fossil fuels and its need to purchase out-of-state energy, as well as provides emergency load reduction.
Project Specifics Contractor: Antelope Valley Water Storage, LLC Partners: Energy and Environmental Economics, Inc; GEI Consultants, Inc; HDR Engineering, Inc; and Water and Energy Consulting Amount: $1,000,000 Co-funding: $225,000 from Antelope Valley Water Storage, LLC Term: March 2017 to December 2018
ATTACHMENT 4 Project Narrative Form
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1. Technical Merit and Need a. Goals, objectives, and innovation - Why is this Project Important
The vision of this project is to use the energy embedded in stored water to seasonally shift electric load and provide emergency demand response. It is important because existing infrastructure is currently underutilized to provide multiple energy benefits. This project will remove the barriers and promote California’s broader energy goals. The project would develop demand response and load shifting tools and strategies to manage load, minimize peak demand, and reduce energy costs in the water sector. Goals: what this project will achieve
Benefit IOU ratepayers: greater reliability, lower cost, and increased safety Overcome barriers to achievement of the state’s energy goals Increase market penetration of distributed renewable generation
Objectives: how the goals will be accomplished - Peak Load Reduction Reduce the amount of State Water Project (SWP) water delivered during the peak summer months to shift the electric load used for pumping. This shift will occur regardless of whether it is a wet, normal, or dry water year. It addresses the issue of how to meet peak summer loads with an increasing proportion of renewable energy. It also increases the value of hydrokinetic power by moving it from a period of shortage to a period of surplus. - Avoided Renewable Curtailment Shift the pumping for water deliveries into the fall, winter and spring months when over-supply of renewable energy is expected. This will absorb surplus renewables to improve its distributed penetration and reduce the risk of over-generation. This increases the economic competitiveness of renewable generation. - Load Following and Ramping for Renewable Integration Provide reliable and predictable load following and ramping that can be timed to reduce morning and evening ramping requirements and reduce the amount of flexible natural gas generation that must be online and at minimum load during the day (increasing curtailment of solar generation). This provides flexibility without the safety risks and greenhouse gas emissions associated with natural gas combustion turbine plants. This improves the reliability of sustainable power systems. - Emergency Demand Response Use the energy embedded in stored water to provide load reduction in the event of a grid emergency. This enables a shutdown of some of the SWP pumping until the emergency is over, providing dispatchable demand response. This improves the reliability of sustainable power systems and increases renewables penetration. - Onsite Renewable Energy Groundwater banks need energy to extract water. There is an opportunity to provide renewable energy onsite such as solar arrays, wind, and hydropower to create sustainable power systems. Water bank land can be used for dual purposes. It is needed to make the replacement storage equivalent to existing surface water storage. It also enables technologies that can be duplicated at multiple groundwater bank locations. Innovations
i. Water delivery shift Incentivize SWP contractors to shift pumping for water deliveries out of the peak summer months and into a period of likely energy over-supply in fall, winter, and spring months. This reduces peak loads without the need for new combustion turbines or batteries.
ii. Guaranteed load reduction Develop a method using existing infrastructure to address the evening ramp up issue that does not utilize natural gas or batteries. SWP pumps can be shut off rapidly, providing very rapid response to the evening ramp up.
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iii. “Green” replacement storage Implement a novel way to absorb more renewables from distributed sources that uses existing infrastructure plus environmentally-friendly groundwater storage that is not vulnerable to algae blooms. The total energy needed for imported water delivery is not reduced, just shifted in time via storage.
iv. Reduced blackout risk Develop a method to provide dispatchable demand response that can last for days in the event of a grid emergency. Load can be reduced rapidly by shutting down SWP pumps. It can be implemented any time of the year. This provides unique benefits over limited-duration batteries and natural gas turbines.
v. Dual purpose facilities Develop the opportunity to generate renewable energy at existing and planned groundwater banks with dual purpose facilities. This will include hydropower, wind, and combined solar arrays with percolation ponds. Onsite renewables will neutralize the cost of energy to extract water and make the bank equivalent to gravity surface storage.
b. Breakthroughs that overcome barriers to the state’s statutory energy goals.
The State Water Project (SWP) is California’s largest user of electricity. Pumping imported water over the Tehachapi Mountains involves a 2,882’ lift at the four Valley String Pumping Plants and requires over 1,000 mega-watts (MW) of electrical power. This is about 2% of the state’s anticipated 2020 managed peak load of 47,000 MW [1]. Most SWP facilities are sized to deliver 100% of the SWP contractors Table A amounts. Generally, the system has surplus capacity. Average annual Table A allocations are projected to be about 60% of the system capacity (DWR Delivery Reliability Report, 2013). This surplus capacity is an unused asset unless it can be harnessed. Currently, imported water deliveries occur at a relatively constant rate each month. Water storage can be used to shift deliveries from periods of electric shortage in the summer to periods of surplus in the fall, winter and spring. Existing SWP contracts reinforce this constant delivery practice. The California Department of Water Resources (DWR) already starts and stops SWP pumps daily to optimize pumping. Their monthly delivery schedule, however, is largely determined by the SWP contractors. The contractors focus on making water reliable. SWP contracts incorporate a peaking factor of about 9%. Consequently, DWR cannot do much more energy optimization unless water delivery schedules are altered. The innovation of this project is that contractors would be incentivized to adjust their delivery schedules. It will build on the pumping optimization already practiced by DWR, converting “as available” load reduction to guaranteed load reduction. This optimizes energy as well as water benefits. Contractors that recharge groundwater basins would shift recharge deliveries out of the summer months. Shifting recharge deliveries is straightforward and reduces the flow that must be pumped over the mountains during peak summer hours. Large surface reservoirs would also be drawn down in the summer months and refilled in the non-summer months. Willow Springs Water Bank (WSWB) has the advantage of being able to offer replacement storage volume for existing surface reservoirs, allowing them to be used for energy benefits. WSWB’s replacement storage will provide water reliability that is equivalent or better for participating agencies.
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The first three objectives of this project are based on the California Public Utilities Commission (CPUC) staff white paper entitled “Beyond 33% Renewables: Grid Integration Policy for a Low-Carbon Future”. The white paper is a road map for how the state will achieve 50% renewables by the year 2030. The white paper identified signposts of potential reliability and economic impacts of achieving the state’s energy goal. These signposts include growth in peak load, the evening ramp up, over-supply issues, and the need for ancillary services. E3 studies “Investigating a Higher Renewables Portfolio Standard in California”1, “Western Interconnection Flexibility Assessment”2, and “SB 350 Regional Integration Study”3 all support the value of and need for flexible resources to enable a low carbon, high renewables grid. The last two objectives of this project are unique to WSWB. The emergency demand response is in anticipation of a grid emergency such as the loss of a major generating or transmission facility. Most or all of the units at Edmonston and the other Valley String pumping plants could be shut down. Water demands would be met by drawing down storage. If all 12 maximum operating units at Edmonston are pumping, this is a load reduction of 1,056 MW. A 6-unit shutdown is about 530 MW (6-7 units on average are used in a normal year). The shutdown can last for a number of days based on the amount of water in storage. This emergency demand response improves renewables penetration by providing firm load shedding to complement variable renewable supplies. The final objective of generating renewable energy onsite builds on the fact that WSWB can incorporate dual purpose water banking and renewable energy generation. There are already roughly 110 MW of solar arrays on 640 acres built out at WSWB. No more solar arrays can be built, however, unless they are located in the wetted areas of percolation ponds. This grant funded project will determine how much renewable energy can be generated through the construction of more solar arrays, including on the wetted area of the percolation ponds. The site also has the potential for 6-12 MW of hydropower from pumped storage. This is the subject of a previously awarded CEC grant (EPC-15-049). This new study will develop enough renewable energy onsite to make the bank energy neutral, i.e. it generates as much energy as it uses to extract water. It will provide a model for how groundwater banks at other locations might be able to add renewable energy generation to their existing water banking functions. Other barriers to optimizing delivery schedules are institutional and legal structures (Figure 1). Institutionally, an innovative structure is needed that links the Investor Owned Utilities (IOUs), DWR, the SWP contractors, and WSWB. This project will develop those structures. Legally, SWP contracts need to be amended to provide the flexibility to shift water deliveries out of the summer window. This project will address those contractual issues. This applied research and development project will develop the technologies, tools and strategies needed to incentivize this delivery shift and overcome the barriers. It will also provide the background information needed by the CPUC to make their solicitation process with the IOUs flexible enough to realize this opportunity. Finally, it will develop the organizational structures and legal concepts needed to implement these incentives.
1 https://ethree.com/public_projects/renewables_portfolio_standard.php 2 https://ethree.com/public_projects/western_interconnection_study.php 3 https://www.caiso.com/Pages/documentsbygroup.aspx?GroupID=4C17574F-73AE-40E3-942C-59C3A13BBDF1
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It is understood that changing the status quo for how imported water is delivered will not be easy. That is why this EPIC-funded project is needed. Without it, the potential energy benefits that could be harvested from existing infrastructure might go unutilized.
Figure 1: Water/Energy Bank Institutional Structure
c. Current status of the relevant technology
Currently there is little incentive for SWP contractors to shift recharge deliveries out of the summer window. There is also no incentive for agencies with control over large surface reservoirs to do the same thing. This project would change the status quo by developing the necessary incentives. There would not be a significant change in the amount of water delivered annually, just a shift in the monthly pumping. DWR currently charges contractors for the cost to transport water in the California Aqueduct. This charge is a pass through and is primarily due to energy costs. A reduction in DWR’s transportation charge could be realized if pumping is shifted to periods of lower electric rates. This potential reduction needs to be calculated. Not knowing the amount of the potential cost savings makes it difficult for a contractor to see that a delivery shift is in their best interests. Existing SWP water infrastructure are the primary facilities involved. This technology is well-understood. Use of existing infrastructure reduces the environmental impact of new generation facilities and makes better use of existing transmission facilities. Groundwater banking is also a well-established practice. Existing groundwater storage banks would be used; no new banks would be built. The one area that involves new technology would be the potential placement of a solar array within the wetted area of a percolation pond at the WSWB site. To our knowledge, this has not been done anywhere. If we are successful, it will increase the number of locations that solar arrays can be built by enabling dual purpose facilities.
d. Need for EPIC funding. EPIC funding is needed to change the status quo. SWP contractors need an incentive to shift water deliveries. This is a barrier to realizing the potential energy benefits. This project would
DWR WSWB
Replacement Storage to Shift SWP Deliveries
Funding from Solicitation
Shift Electricity Use
IOU
SBVMWD
MWA
AVEK
MWD
Others
SWP Contractors
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develop those incentives. The benefits of lower DWR transportation costs need to be quantified and made transparent. Information will trigger the enlightened self-interest of the contractors who are able to shift their delivery schedules easily. There are also structural barriers. The cost of building out groundwater storage to replace surface water storage needed for delivery shifts should be eligible for monetization under CPUC and IOU solicitations for new energy sources and ways to meet energy needs. This project will assess how that can be accomplished. Additionally, there are information barriers. The delivery shift being proposed is not currently envisioned in IOU solicitations. The proposed work will collect the information needed to enable the CPUC to incorporate the potential for water delivery shifts as a more reliable, lower cost, and safer way to meet energy needs. This concept is not being developed by any sector right now because it involves multiple parties and multiple sectors (water, energy, and government) to make it work. It also involves public and private interests. Electric Program Investment Charge (EPIC) funding is needed to bring these diverse interests within the IOU service areas together synergistically. Active participation by DWR, SWP contractors, the CPUC and CAISO, and others will be sought and welcomed.
e. Technical feasibility. This project relies primarily on existing SWP infrastructure and water banks. The major impediments are legal, institutional, and informational. SWP contracts must be amended to encourage water deliveries during periods when it optimizes both water and energy benefits. Contractors must be confident that their water reliability will not be compromised, that annual deliveries remain the same, and that their costs will be reduced. Institutional structures must be developed so that DWR and the IOUs can take full credit for the energy benefits realized. This project is beyond basic research. It will involve the participation of agencies needed to realize the energy savings. We need to have them tell us how best to implement this project. Lack of information is a significant impediment. An information gap exists in how much load reduction can be obtained from a shift in water deliveries. DWR already optimizes pumping to the extent they can. They cannot, however, adjust the imported water delivery schedule. Typical daily pumping operations are shown in Figure 2, which shows the daily pumping pattern for two randomly selected days in 2013. The optimal operating scheme is to have a 12-pump flow at night and shut off all pumping units during the peak hours from about 2:00 p.m. to 8:00 p.m. Between the periods of maximum and minimum pumping, there are ramp down and ramp up periods. DWR normally starts and stops Edmonston units in 2-pump increments. Sometimes DWR is able to achieve nearly optimal pumping, as was the case for August 1, 2013. However, when delivery schedules force some pumping during the peak, they must pump during the peak hours (see July 1, 2013 in Figure 2). An objective of this project is to determine how much additional electric load reduction is possible using a delivery shift. Delivery shifts come from changing the recharge delivery schedule and drawing down storage. The potential load shift will be estimated by consulting with DWR staff and SWP contractors, examining historical records, and determining how much replacement storage is needed to enable a seasonal load shift. A comparison of two days in 2013 on Figure 2 suggests that 371 acre-feet of delivery shift could have enabled a 2-pump shut
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down for 5 hours and a 4-pump shut down for 1 hour on July 1. A 2- to 4-unit pump shut down enables a load reduction of 176 to 352 MW. This delivery would be shifted to non-summer months. A preliminary assessment of DWR pumping data for the summer of 2012, a 65% Table A allocation year (normal), indicates that a total of about 54,000 AF could have been shifted if storage drawdown enabled DWR to further optimize its pumping. This estimate is based on actual DWR pumping records over the past 5 years (obtained through personal communication with DWR). This would have resulted in about 320 MW of summer peak load reduction for a normal year. Wet years result in greater amounts of potential load reduction by shifting deliveries. Detailed data analysis of dry, normal, and wet year pumping patterns will be part of this project. In an extremely dry year, such as 2014 (5% Table A), little load shifting is possible. DWR already optimizes pumping. This does not impact the potential load shift of this project because when pumps are completely shut off in an extremely dry year they do not create any load.
Figure 2: Selected Edmonston Plant Daily Operating Data for 2013
f. Measurement and verification plan. Project goals and objectives will be achieved by using water storage to shift the timing of when water is pumped to Southern California. Water agencies that currently recharge most of their SWP deliveries will be incentivized to recharge only during the fall, winter, and spring months. Large surface water reservoirs would be provided replacement storage from Willow Springs Water Bank. Replacement storage must provide equivalent or better water reliability and cost. Energy shifted can be quantified by measuring the volume of water deliveries shifted with its associated embedded energy.
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Water pumped over the Tehachapis has 3.2 MWh/acre-foot embedded in it [2]. This embedded energy is straightforward to measure and track. The number of acre-feet shifted out of the summer window is measurable. For example, a 54,000 acre-foot shift out of the three summer months is a 173,000 MWh load shift based on the 3.2 MWh embedded energy. On many days, DWR already optimizes pumping by dropping flows to zero during peak hours. The target of this project is to use storage drawdown to enable more days of optimal pumping. The 320 MW potential load shift estimated for 2012 is a conservative estimate because it does not include recharge delivery shifts. When recharge shifting is included, the load shift potential will be greater. This study will determine how much. The increase in electricity use during over-supply and over-generation risk periods is also quantifiable through measurement of the volume of water deliveries shifted to the non-summer seasons. A reduction of 173,000 MWh in summer energy use corresponds to an equivalent increase in energy use during months of anticipated over-supply. There is no net change in the total amount of energy used. A shutdown of some SWP pumping units that convey water over the Tehachapis could also enable emergency demand response by shedding load. Water demands will be met by drawing down storage. It would take about 3,850 AF per day of drawdown from surface reservoirs to enable a 6-pump load reduction. A 7-day outage would take 27,000 AF of water storage drawdown. The load reduction would be 530 MW for a week. This improves grid reliability in the event of a black swan event such as the loss of a major generation or transmission facility or an unexpected setback like the Aliso Canyon gas leak. Capacity in WSWB can be used to temporarily meet the delivery needs of SWP contractors that cannot switch to taking deliveries out of storage in surface reservoirs. Quantification of these energy savings will be with respect to the following criteria:
1. Peak summer load reduction per acre-foot of deliveries shifted, in MWh/acre-foot 2. Predictability and certainty of demand reduction during the evening ramp up period,
in MW (pumps can be shut down in minutes) 3. Off peak energy use increase during periods of expected surplus, in MWh/acre-foot 4. Decreased greenhouse gas creation from using more renewables during over-supply
periods, in CO2 tons/year 5. Emergency demand response, in MW for a given number of days 6. Renewable energy generated at the WSWB site, in MWh
All of these criteria will be tracked over the course of the project. As information is developed and results of the applied research become available, the quantification of these benefits will be updated and verified.
g. California Environmental Quality Act (CEQA) compliance Most of the infrastructure involved is already built. WSWB had its Environmental Impact Report approved by Kern County in 2006. No additional CEQA documents are necessary.
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h. GFO-16-305 Group 2 Projects The project fits within GFO-16-305 Group 2 projects for “Advancing Cutting-Edge Technologies and Strategies to Reduce Energy Use and Costs in the Industrial, Agriculture and Water Sectors”. The project is applied research and development and develops strategies to facilitate load shift and manage peak load in response to demand response and price signals. It will assess the conversion of hydrokinetic energy used for pumping water over the Tehachapi Mountains into hydrostatic (potential) energy and has the potential to shift up to 100% of the peak hour demand in the summer months. The hydrokinetic energy is created by the pipes and pumps of the California Aqueduct. This kinetic energy of water in motion is converted into hydrostatic energy that is embedded in water stored in both the groundwater basins and surface water reservoirs (Figure 3). Embedded energy is released when the stored water is used consumptively. Effectively, the water is “pre-pumped” over the mountains. This project is beyond basic research and does not require the construction of large dams or reservoirs, new water banks or otherwise require diversions from natural waterways. It will also use the existing electric transmission system better because use of existing facilities for load shifting does not require new transmission capacity. The only additional facilities needed are to finish the buildout of the existing WSWB groundwater bank, which has already been approved under CEQA. No change in total annual amount of SWP water deliveries is required. The project will include the development of protocols and procedures that provide tools and strategies to incentivize water agencies to shift their imported water delivery schedules. Most of the barriers are institutional and informational. New facility requirements are modest because of the reliance on the existing SWP infrastructure. The unique advantages of using a water/energy bank for demand response and peak load reduction include:
Use of more renewable energy by shifting load to a season when renewables are in surplus (combustion turbines and batteries cannot do this)
Rapid and predictable daily load shedding during the evening ramp up period Facilities needed are already built or already authorized under CEQA The potential for dual use of the water bank site to develop more solar power and
pumped storage hydroelectric power. Groundwater basins that may participate include the Antelope Valley, the Mojave Valley, and the San Bernardino Valley. Surface water reservoirs that may participate include DWR’s Castaic Lake (319,000 AF) and Lake Perris (127,000 AF). Water would be pre-delivered to these reservoirs and then drawn down in the summer. Metropolitan Water District of Southern California (MWD) has operational control over most of the dry year storage in Castaic and Perris. Their concurrence is an important step if cycling these terminal SWP reservoirs is needed to realize energy benefits. Replacement storage must be provided to enable use of existing surface storage for energy benefits. This is because the reservoir might be drawn down for energy purposes when the water in storage is needed to meet dry year needs. WSWB is planned for a capacity of 1,000,000 AF. It is partly built out. Some of the future capacity must be allocated to meet the needs of existing customers and to provide public benefits under Proposition 1. The remainder of the bank’s capacity is available to meet water and energy needs.
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Groundwater storage needs energy to extract water. To make groundwater storage equivalent to gravity surface water storage, the energy needed to extract water must be provided from renewable sources. This is why the assessment of onsite hydropower and solar energy is necessary. Groundwater storage at WSWB and surface water storage in the Southern California coastal plain are not inherently equivalent. WSWB is north of the San Andreas Fault. This makes it less desirable for emergency storage. As long-term dry year storage, however, groundwater storage should be preferable. This is because each acre-foot of firm put and take capacity in WSWB corresponds to 3 to 4 acre-feet of new storage volume. This improves the reliability by increasing volume of water available for dry year yield. Also, groundwater storage does not evaporate each year (surface water reservoirs typically lose 5% annually) or has seasonal water quality issues such as toxic blue-green algae blooms.
To the extent possible, DWR should control the optimization of operating the pumps and storage. This will reduce coordination problems. DWR already does a good job of optimizing SWP pumping based on the delivery schedule they are given. The incentive to shift imported water deliveries will give them the additional tool they need to further optimize energy use.
This project can serve as a template for how other large, pumped aqueduct systems in California may be able to use storage to optimize conversion of hydrokinetic and hydrostatic energy. Generally, all that is needed to replicate this concept is periodic surplus conveyance capacity and access to storage. For example, the Colorado River Aqueduct (2.0 MWh/AF
Fall, Winter and Spring Flow Increase
Draw Down
San Luis Reservoir
Edmonston
54,000 AF
Recharge Contractors
Summer Flow Reduction 0 AF
Edmonston
Leave Full
Surface Storage with 3.2 MWh/AF embedded
San Luis Reservoir
Surface Storage drawn down
Figure 3: Water/Energy Bank Shift of Embedded Energy
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embedded), or the Los Angeles Aqueduct (1.5 MWh/AF energy generation potential) may be able to improve the timing of pumping or power generation if similar incentives are developed. Lessons learned will be incorporated in the final report. The incentives that are successful will be particularly emphasized. These can help other aqueduct systems determine how much of this project may be directly applicable to their situation. Project partners and stakeholders such as DWR, the SWP contractors, CEC, CPUC, CAISO, and others will be consulted for the best way to convey these lessons learned to large aqueduct systems that may benefit.
2. Technical Approach
a. Technique, approach, and methods - What will we be doing?
The project will be conducted in 6 major tasks: (1) Contractor Outreach: meet with SWP contractors and determine what incentives they
need to shift their delivery schedules. The needs of the contractors who primarily recharge imported water will be different from the needs of contractors and water agencies that have existing surface storage reservoirs for imported water storage. This will include the development of a strawman set of incentives to provide “proof-of-concept” if accepted by the SWP contractors.
(2) DWR Operations: coordinate with DWR to determine the extent to which a shift in the SWP delivery schedule can enhance current operations of DWR’s Valley String Pumping Plants and reduce transportation costs via lower electric rates. Also, assess the potential to leverage the energy benefits by adjusting when deliveries are shifted.
(3) Reservoir Operations: assess what is needed to make storage in a groundwater bank equivalently reliable when compared to storage in a surface water reservoir. Also assess the low point mitigation benefits from leaving more water in San Luis Reservoir storage during the summer months and replacing it during the other months.
(4) Electric Grid: assess the benefits of a guaranteed imported water delivery shift for the electric grid. IOUs can use this to avoid building new combustion turbines and batteries. An institutional structure needs to be developed to link all of the participants and provide the financial incentives needed to shift imported water deliveries.
(5) Economics: quantify the economic benefits of reduced peak summer electric load and increased load during periods of expected surplus, including the avoided cost of facilities needed to meet summer peaks, the reduction in the SWP transportation charges, and the increased penetration of renewable energy.
(6) Onsite Renewables Generation: assess how much additional renewable energy can be added at the water/energy bank site to supplement the existing solar arrays that are already installed at the WSWB site.
Each task is described in more detail in Attachment 6, the scope of work.
b. The project manager will coordinate all of the individual tasks. WSWB staff will provide the project management. Microsoft Project will be used to keep the project on time. Internal accounting and budgeting controls will be used to keep the project on budget. The separation of the scope into discrete but coordinated tasks will leverage the capabilities and unique skills of the project team.
c. Success Factors.
Factors critical for success include:
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(1) Are the incentives adequate to trigger contractors to shift their delivery schedules and
can they be packaged into a strawman set of incentives that will trigger a guaranteed delivery shift?
(2) How much replacement storage will be needed and how can it be made equally or more reliable than the surface storage being replaced?
(3) What is the tradeoff between providing water storage to enable peak load reduction versus providing water storage to enable emergency load reduction for the electric grid?
(4) How can the CPUC and the ISO incorporate this potential project into their planned solicitations?
(5) Who will get credit for energy benefits realized by DWR’s reduced summer pumping and for the improved emergency response?
The plan to address these issues includes extensive outreach to the targeted SWP contractors, creation of a strawman incentives package to determine if it is adequate to ensure guaranteed shifting of imported water out of the summer window, discussions with the CPUC, CAISO, and IOUs to determine how best to incorporate this concept into their solicitations process, and outreach to DWR to understand their current operational practices and determine how a shift in imported water deliveries can be optimized to improve energy benefits. Other risks, barriers, and limitations include the lack of contracts that enable SWP deliveries to be shifted, the lack of precedent for a water/energy bank, and the natural hesitancy among water agencies to try something new that might be perceived to result in less reliability. Contractual issues and lack of precedent can be overcome with a successful proof-of-concept process. Hesitancy on the part of water agencies can be addressed with a phased implementation process that proceeds in stages, as well as creating an approach that does not rely on the participation of any one water agency. An incentive for contractor participation is likely to be the calculation of how much the DWR transportation charge will be reduced by a delivery shift. The current charge for much of Southern California is about $250/acre-foot. It is largely composed of energy costs. If DWR could be sure of a monthly delivery shift, they could shift electrical use to a period when it is less expensive. It should result in a significant costs savings for the impacted contracts. Because transportation charges are calculated after the water year is over, the financial benefit would have to be estimated in advance.
d. How knowledge gained will be made available to the public & decision-makers. The final report will include recommendations on how the findings can be implemented by the California Energy Commission (CEC), CAISO, CPUC, DWR, and the SWP contractors. The report and related documents can also be posted on the CEC website to facilitate information transfer. WSWB will develop the online tools and related documents needed to convey project results to a much wider audience. These tools can also be installed on the CEC website for greater public and professional access. If the opportunity is available, the results can also be presented at professional conferences and may also take the form of journal articles.
e. Scope of Work and Project Schedule Included in Attachments 6 and 6a.
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3. Impacts and Benefits to IOU Ratepayers
a. Ratepayer benefits – How will California IOU Ratepayers Benefit?
Both the WSWB and the existing California Aqueduct system are located within California IOU service areas. WSWB is within Southern California Edison and the California Aqueduct is within SCE and PG&E service territories. Greater reliability Improved reliability for the electric grid will result from a guaranteed summer shut down of SWP pumping units. This provides a firm source of demand management for the grid that is independent of whether the water cycle is wet, normal or dry. It provides rapid and predictable demand reduction that can be timed to match the daily evening ramp up period anticipated as solar arrays go offline. Reliability is enhanced by the fact that there is no reliance on natural gas combustion turbine plants, which are subject to availability concerns. With the loss of the Aliso Canyon natural gas storage facility, new methods to meet summer peaks are needed. Ratepayer reliability is also enhanced by the capability to shut pumps off for days during grid emergencies. This demand response can be dispatched rapidly at any time by allocating some water storage to emergency load reduction. This is not constrained by the 4-hour maximum discharge period of most batteries. This can be implemented without the fossil fuel consumption, safety issues, and costs associated with combustion turbines. This will reduce the risk of blackouts if a major generation or transmission facility fails. Emergency demand response for very long durations is a unique feature of this proposed project. Lower Costs The capital cost to meet peak electricity needs using new combustion turbines or batteries will be avoided with summer shut downs of the SWP pumps. DWR transportation costs will be reduced by using the lower rates for electricity available during the non-summer months. This will be passed on to IOU ratepayers because the water agencies benefiting from the lower costs are within IOU service areas. Lower costs may also result from the lower costs associated with utilizing water storage for peak load reduction compared to the cost of building a new combustion turbine. A 320 MW combustion turbine costs roughly $450 M ($1.4 M/MW [3]). Groundwater storage costs less than a new combustion turbine. Also, it does not include any additional costs that may be needed to make the delivery of natural gas safer. Increased safety Increased safety results from having a source of peak summer and emergency response power that does not involve natural gas combustion turbines. It is not subject to safety issues like the natural gas leak at Aliso Canyon and explosion at San Bruno. This increased safety will be passed on to IOU ratepayers because most of the natural gas combustion turbines needed to meet summer peaks are located within ISO service areas. This increased safety is especially important as California moves from less energy generated by fossil fuels and nuclear power and into a future that incorporates more renewable energy. The water/energy bank is a viable option for reducing the amount of peak energy needed from natural gas combustion turbines. As shutdowns of the San Onofre and Diablo Canyon nuclear power plants (planned in 2025) and phase-out of once-through fossil fuel plants occur, the state would not need to build as many new combustion turbine plants with the associated safety risks.
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b. Quantitative estimates of potential benefits to California IOU ratepayers
Table 1: Estimate of Potential Benefits Benefit Quantity Justification
1. Peak summer load reduction
320 MW Shutting down pumps at Edmonston during the peak summer hours by shifting deliveries
2. Instant power for evening ramp up
Within minutes
Pumps can be scheduled to start and stop to match evening ramp up as solar arrays go offline
3. Increased use of renewables
173,000 MWh
Shifting deliveries into the period of over-generation risk enables increased electricity use
4. Reduced greenhouse gases (GHGs)
94,000 metric
tons/yr. of CO2e
GHG reduction due to 173,000 MWh load shift to the over-generation risk period. Assuming that the heat rate
(therm/kWh) is 0.1027i, and emissions factor (CO2e) is 0.0053 metric tons/thermii.
5. Emergency demand response
530 MW Shut down 6 units at Edmonston plus 3 other Valley String pumping plants for 7 days
6. Avoided cost of building a new combustion turbine.
$450 M Utilizing groundwater storage for peak load reduction instead of building a new combustion turbine [3]
7. Increased onsite solar energy
110 MW Add solar arrays on another 640 acres at the WSWB. Roughly 110 MW of solar is already installed at WSWB
8. Onsite hydropower
6-12 MW Estimated hydropower that can be realized by building pumped storage at the WSWB (EPC-15-049)
c. Timeframe, assumptions, and calculations for the estimated benefits
The project can be implemented once WSWB is fully built out. This is expected in the year 2020 based on the availability of anticipated water bond grant funding: WSWB expects to be awarded grant funds to help with its buildout and these funds will not be available until 2018. A 2-year construction period is expected. Existing SWP infrastructure and existing recharge facilities are already available. WSWB has been partially operational since the year 2011, when it recharged about 20,000 acre-feet. It operates under the constraints of a Memorandum of Understanding with Kern County, which defines the operating criteria needed to ensure the water bank does not have a negative impact on any of its neighbors. The groundwater basin was adjudicated in 2015. These factors make the timeframe for realizing the anticipated benefits reasonable: we are simply completing the build-out of an existing facility which is predictable and well-understood. Benefits will start to accrue as soon as agreements are in place to shift water deliveries. This can be as early as 2020. Benefits listed in items 1 through 6 in Table 1 can begin at that date. Implementation of more renewable energy onsite at WSWB such as a solar array placed in the percolation ponds will take longer because the facilities needed would require CEQA, planning, design, and construction before the benefits can start. This is estimated to take up to 5 years.
d. Impacted market segments. This project impacts the renewable energy, natural gas, and water market sectors.
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Electricity The electricity sector will be enhanced because the project will reduce electricity demand when renewable energy may not be able to meet peak loads. It will increase demands to soak up surplus renewable energy when there is a risk of over-generation. 173,000 MWh of renewable energy is estimated to be shifted to periods of over-generation. Any renewable energy generated at the water bank site will add to this total. The ability to provide emergency demand response will also enhance the energy sector by reducing the risk of blackouts. This is consistent with the goals of the EPIC program. More renewable energy use will result in more renewable energy jobs. This is consistent with the Governor’s Clean Energy Jobs Plan (2011). It is also consistent with SB 350, the Clean Energy and Pollution Reduction Act of 2016. Natural Gas The natural gas sector is impacted by a reduced need for summer deliveries to supply combustion turbines. This will be equivalent to the amount of natural gas expected to be used by a combustion turbine, including the natural gas needed for start-up and shut-down inefficiencies. This improves safety for IOU ratepayers by reducing the chance of natural gas incidents like Aliso Canyon and San Bruno. It also reduces greenhouse gas creation by the natural gas sector to meet peak electric needs. This is consistent with AB 32, the Global Warming Solutions Act of 2006, and Executive Order B-30-15 to reduce greenhouse gas emissions. Water the water sector impacts will be addressed by ensuring that replacement storage provides equal or better reliability and at the same cost. The storage volume needed to do this is estimated at 500,000 to 1,000,000 acre-feet of new storage from WSWB. An additional water benefit is the mitigation of water quality problems in San Luis Reservoir. This occurs because water deliveries out of San Luis Reservoir will be shifted to the non-summer months. Water and energy savings by the water sector is consistent with Executive Order B-30-15 to achieve water and energy savings and greenhouse gas reductions.
e. Qualitative or intangible benefits. This project provides a rapid response to the need to rely less on natural gas to meet electricity needs. With the problems at Aliso Canyon and San Bruno, the use of natural gas at combustion turbines may be impacted. Additionally, shutting down or turning on electric pumping units at an existing facility is inherently more efficient than starting up a combustion turbine. It also does not involve the wasted fossil-fuel energy during start up and shut down. The proposed project involves existing infrastructure plus environmentally-friendly groundwater banks. This makes the implementation time frame extremely rapid. Groundwater banks are “greener” than an equivalent volume of surface storage because they do not flood lowland habitat, do not flood Native American and archeological sites, and do not require the construction of major new dams. The project reduces summer water drawdown at San Luis Reservoir to improve water quality when low water levels cause algae blooms. Toxic blue-green algae blooms are becoming more common as levels of carbon dioxide increase. This project addresses a public health issue brought on by the drought and climate change and will create water supply benefits as well as energy benefits. Specific qualitative benefits include:
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Economic development Use of existing water infrastructure to meet energy needs reduces the cost and time of implementation. It also reduces the need to purchase energy from investor-owned utilities or sources outside of California during the summer months. Additionally, increased penetration of renewable energy will provide more renewable energy jobs in California.
Environmental benefits Increased penetration of renewable energy and less use of combustion turbines to meet summer peaks reduces greenhouse gas creation. It also decreases California’s dependence on fossil fuels. Replacement storage would be provided from environmentally-friendly groundwater storage, which also provides a site for additional renewable energy.
Public health Leaving water in storage in San Luis Reservoir during the summer months mitigates algae problems that occur during periods when the volume of water in the reservoir drops below 300,000 acre-feet. Algae blooms cause taste and odor problems and may involve toxic blue-green algae.
Consumer appeal Use of existing infrastructure better avoids the construction of new dams or new diversions from waterways, reduces reliance on natural gas, and avoids the construction of new combustion turbines. This should appeal to consumers. It also reduces the chances of electrical outages by providing dispatchable demand response.
Energy security Increased use and penetration of renewable energy during periods of anticipated over-supply and over-generation reduces California’s dependence on fossil fuels and its need to purchase out-of-state energy, as well as provides emergency load reduction. f. Cost-to-benefit analysis- What is it going to cost ratepayers and is it worth it?
Buildout costs for WSWB total about $200 M, enabling ~320 MW of regular load shifting capability and up to 1,056 MW of emergency load reduction. This is less than the cost of a 320 MW combustion turbine of about $450 M; an equivalent battery would cost more. E3 studies find that the primary benefits of flexible loads is not in providing peaking capacity, but in providing load following for morning and evening ramps and preventing curtailment of renewable generation. Studies performed by E3 for utility scale energy storage find annual benefits of avoided curtailment, reduced start-up costs and reduced fuel and O&M savings of $50 to $110 million for a 320 MW plant. These are calculated for low and high value scenarios developed by E3, used most recently in the CAISO SB 350 Regional Integration study.4 On the higher end of benefits, a simple payback is achieved in less than two years. As part of this study, E3 will further quantify the benefits this project provides for the electric grid and California Ratepayers using well-established models and methods used for the CPUC, CEC, CAISO and California IOUs. If the capability to provide load following and ramping is assumed to have the value of a combustion turbine, the benefit/cost ratio for the proposed project would be 2.25. If the anticipated 50% Proposition 1 grant is obtained in return for WSWB water storage benefits, this ratio would double. More precise benefits/costs analysis will be performed as part of this project. The additional value for more than 320 MW of load shifting during wet years and due to shifting
4 See Volume 4, Published July 21, 2016 and available on the CAISO website: https://www.caiso.com/Pages/documentsbygroup.aspx?GroupID=4C17574F-73AE-40E3-942C-59C3A13BBDF1
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of recharge deliveries will also be evaluated as part of the project. This will further increase the benefit/cost ratio. Benefits due to increased renewables penetration will also accrue. They result from the avoided cost of renewables integration, avoided cost of electric transmission, and the avoided cost of alternative natural gas transmission to generate peak energy. The Antelope Valley is the center of numerous solar and wind generation facilities, making it a good location to integrate more renewable energy. These benefits will be estimated as part of the project. The benefits of emergency demand response are also valuable. The ability to reduce pumping at Edmonston during a black swan event would give the electric grid a new tool to improve reliability. This reduces the risk of black-outs and improves the reliability of the renewables portfolio, enhancing penetration. It would be available any time of the year. When Edmonston is using 6 pumping units, this would be 530 MW of immediate load shedding for 7 days. This is a unique feature of this project. Its value will be estimated as part of the project. This project has the potential to return many times its original cost. It can be online rapidly due to its reliance on existing infrastructure. CEQA is complete and there is little technical or financial risk. IOU ratepayers will be the ultimate beneficiaries of these advantages.
4. Team Qualifications, Capabilities and Resources - How will the project be completed?
a. Organizational structure and the project team: Please see Attachment 5 and
Figure 4.
b. Key Team Members: The study will be carried out by 7 key team members, of whom 3 are professional engineers and 4 have masters or PhD degrees. All are experts in their technical areas and are experienced in managing large, complex technical projects. For details, please see the organization chart (Figure 4) and Attachment 5.
c. Qualifications, experience, capabilities, and credentials of team members:
The key team members’ qualifications, experience and capabilities as applicable to the proposed study have been provided in Attachment 5, Project Team Form.
d. Management and Coordination: The Project Manager, Mark Beuhler, has managed many large and multi-faceted research and development projects, especially during his tenure as the Director of Water Quality at the Metropolitan Water District of Southern California. Project management software and/or spreadsheets will also be used to track progress. The project will take 20 months to complete (see Attachment 6 for project schedule). Tasks will be broken up into 6 complementary and coordinated components. After each task is complete, a technical memo will be written. These memos will form the basis for the final report. Management and coordination of the various tasks will be provided by the Project Manager. A final report will be produced 18 months after notice to proceed. Assuming the project starts in March, 2017 it will be complete by December, 2018.
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Figure 4: Water/Energy Bank Project Team
e. Facilities, infrastructure, and resources available to the team: WSWB facilities
available to the team include 320 acres of percolation ponds with turnouts and meters, 9 irrigation wells with electric hookups, 6 new production wells and 2 miles of 48” to 54” recharge pipelines. The WSWB fact sheet shows maps and photos of these facilities.
f. Team’s history of successfully completing projects: The applicant, Antelope
Valley Water Storage (AVWS), is a subsidiary of CIM Group, LLC. CIM Group currently has $20 billion under management and has 500+ employees. To date, CIM has made over 130 investments, including investments for pension funds such as CalPERS. CIM routinely manages and implements multi-million dollar projects. The subcontractors all have extensive experience in conducting tasks of similar scope and complexity as those described in Attachment 6.This experience is detailed in Attachment 9, Reference and Work Product Form.
g. Past projects that resulted in a market-ready technology: The applicant’s relevant
projects are listed in Attachment 9, Reference and Work Product Form. h. Relevant references: Current references have also been provided in Attachment 9. i. Collaboration with utilities, industries, or others: Extensive collaboration will be
needed for this project. Water agencies such as Antelope Valley-East Kern Water Agency (AVEK), Metropolitan Water District of Southern California (MWD), Mojave Water agency
AVWS
Mark Beuhler, PE
Advisory Committee
DWR, CEC, CPUC, AVEK, SBVMWD, SGPWA, PWD, MWD, etc.
Contractor Outreach
Reservoir Operations
Mark Williamson, PE
Jeffrey Weaver, PE Lon House,
PhD
Economics
Leo Winternitz
DWR Operations
Electric Grid
Arne Olson
Onsite Renewables
Mark Beuhler, PE
Eric Cutter, MBA
Project Economics
CA Electricity Market
CEC
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(MWA), San Bernardino Valley Municipal Water District (SBVMWD), DWR, San Gorgonio Pass Water Agency (SGPWA), and others will all be consulted on their potential participation in the water/energy bank.
j. Respond to the following questions. Include an explanation for any “yes” answer:
o Has your organization been involved in a lawsuit or government investigation within the past five years? Yes, AVWS has been involved in an eminent domain lawsuit with SCE over the past 6 years. The dispute is over the value of an easement that SCE acquired from WSWB.
o Does your organization have overdue taxes? No. o Has your organization ever filed for or does it plan to file for bankruptcy? No. o Has any party that entered into an agreement with your organization
terminated it, and if so for what reason? No. To our knowledge, no party has terminated an agreement with Antelope Valley Water Storage, LLC.
o For Energy Commission agreements listed in the application that were executed (i.e., approved at a Commission business meeting and signed by both parties) within the past five years, has your organization ever failed to provide a final report by the due date indicated in the agreement? No.
k. Commitment and support letters. Three support letters and two commitment letters have been provided in Attachment 11.
l. The project will be managed by the Prime as discussed in 4d. The proposal for proof-
of-concept is broad and involves many diverse disciplines because of which the requisite expertise is unavailable at any one organization. The proposal has laid out an approach that brings together the best experts from a variety of fields. AVWS will handle all the coordination and management tasks and also serve as the lead on several of the technical tasks (Table 3).
5. Budget and Cost Effectiveness
a. Reasonableness of the requested EPIC funds: The requested funding of
$1,000,000 is 0.22% of the $450 M cost of a 320 MW combustion turbine that the project would obviate. The project will result in improved renewables penetration, improved safety, and increased reliability. The value of these benefits will be quantified during the project.
Table 2: Water/Energy Bank Proof-of-Concept Budget
Task (by major task) Energy Commission
Funds ($)
Match Share ($)
Total ($)
1. General Project Tasks 79,000 0 79,000
2. Contractor Outreach 175,000 0 175,000
3. DWR Operations 150,000 0 150,000
4. Reservoir Operations 175,000 0 175,000
5. Electric Grid 200,000 0 200,000
6. Economics 150,000 0 150,000
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7. Onsite Renewables 0 200,000 200,000
8. Advisory Committee 0 25,000 25,000
9. Project Benefits Evaluation 19,000 0 19,000
10. Knowledge Transfer Activities 52,000 0 52,000
Totals $1,000,000 $225,000 $1,225,000
b. Reasonableness of costs for direct labor, and non-labor and operating expenses by task: Majority of the costs will be spent on technical tasks. The requested funds will cover AVWS’ direct labor and benefits plus indirect overhead (Table 3). Subcontractor costs are standard hourly rates for each consultant and are well within industry’s standards.
c. Why the hours proposed for personnel and subcontractors are reasonable:
The applicant’s experience with past projects has guided the development of the proposed budget and schedule. The hours proposed for AVWS and subcontractor personnel are typical of those that are required to complete activities similar to the ones given in the Scope of Work. Subcontractor personnel are essential because they possess the diverse expertise that is needed to conduct all aspects of the project. Quantifying the value of flexible load under high renewables is an extremely complex task, but is crucial to demonstrating costs and benefits for California policy makers. The state must evaluate many competing strategies and technologies with different characteristics and significant uncertainty regarding future cost, maturity and performance. This proposed project is unique in providing seasonal load shifting capabilities, which E3 has found to be critical in studies for GHG pathways and 50% renewables.
d. Maximization of funds for technical tasks and minimization of
administration expenses: Whenever appropriate, inexpensive staff such as junior personnel or interns will be used to keep costs down. AVWS will not collect any profit from the study. Match funding will also leverage CEC funds. AVWS will confer with the Agreement Manager on ways to further streamline the process.
6. Funds Spent in California
100% of project funds as well as match funds will be spent in California. This information is included in Attachment 7, Budget Forms.
7. Ratio of Unloaded Labor Costs to Loaded Labor Costs
Table 3 shows the ratio of direct labor and fringe benefits rates to loaded labor rates for both the recipient and major subcontractors.
Table 3: Direct Labor versus Loaded Labor Costs Recipient or Subcontractor Direct Labor
& Benefits Costs ($)
Loaded Labor
Costs ($)
Ratio Tasks
Antelope Valley Water Storage 110,314 148,475 0.74 1, 7, 8, 9,10 Energy and Environmental Economics, Inc.
137,229 249,143 0.55 5,6
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GEI Consultants, Inc 184,528 320,010 0.58 2,3 HDR Engineering, Inc 85,582 173,446 0.49 4 Water and Energy Consulting 90,475 99,566 0.91 6
8. Match Funding
AVWS will contribute staff time needed to field test the combined operation of percolation ponds in conjunction with solar arrays and to assess the onsite wind energy generation potential. To our knowledge, combining percolation ponds with solar arrays has never been done before. It raises a number of operational and maintenance issues that need to be field tested. The estimated value of staff time is $200,000. WSWB will also contribute the $25,000 cost of convening the Advisory Committee. The match funding commitment letter is in Attachment 11.
9. Disadvantaged Communities (DACs) Mojave Water Agency (MWA) is one of the SWP contractors that can potentially shift its recharge deliveries out of the summer window and benefit from this project. MWA has DACs in its service area located near the cities of Barstow, Baker, Apple Valley, Victorville, and Adelanto (SB 535 List of Disadvantaged Communities). Likewise, Antelope Valley-East Kern Water Agency (AVEK) is another SWP contractor with DACs in its service area that can benefit from the project. Finally, the IOU ratepayer benefits resulting from the proposed project will accrue to a wide region of the state, throughout all the three IOU service areas including much of the Central Valley. DACs located in the Central Valley will benefit directly from the improved reliability, lower cost, and increased safety provided by this project. REFERENCES [1] California Energy Commission. 2014. California Energy Demand Updated Forecast, 2015- 2025. Figure ES-4 in http://www.energy.ca.gov/2014publications/CEC-200-2014-009/CEC-200-2014-009-SD.pdf [2] Los Angeles Department of Water and Power (LADWP). 2010 Urban Water Management Plan. Exhibit 12-H in http://www.water.ca.gov/urbanwatermanagement/2010uwmps/Los%20Angeles%20Department%20of%20Water%20and%20Power/LADWP%20UWMP_2010_LowRes.pdf [3] California Energy Commission. 2014. Estimated Cost of New Renewable and Fossil Generation in California. Table 51 in http://www.energy.ca.gov/2014publications/CEC-200-2014-003/CEC-200-2014-003-SD.pdf. ENDNOTES i The heat rate (therm/kWh) is obtained from the heat rate value of 10,268 Btu/kWh for natural gas-fired peaker power plants. Sources: California Energy Commission. 2014. Thermal Efficiency of Gas-Fired Generation in California: 2014 Update. Table 2 in http://www.energy.ca.gov/2014publications/CEC-200-2014-005/CEC-200-2014-005.pdf; QFER CEC-1304 Power Plant Data Reporting ii The emissions factor (CO2e) value of 0.0053 metric tons/therm (5.3 kg/therm) is the standardized emission factor for natural gas. Source: California Energy Commission Energy Resources and Development Division Staff (Attachment 12).
WILLOW SPRINGS WATER BANK CONJUNCTIVE USE PROJECT ELIGIBILITY A6 – OTHER APPENDIX
Appendix C
Created by: Tommy Ta Revised by: Tommy Ta
Created date: 12/27/2017 Revised date: 8/8/2017
Greenhouse Gas Reductions TableSource Metric tons of CO2/year Comments
1. Load shift from water/energy bank 94,000 From GFO‐16‐305 proposal
2. 640 acres of existing solar arrays 70,000 110 MW of existing solar arrays
3. 640 acres of new solar arrays 70,000 110 MW of dual use ponds & arrays
4. GHG created at 0.5 MAF surface reservoir 30,000 From Oct. 2016 BioScience article**
Total 264,000 Equivalent to taking 56000 cars off the road
Module Type: Describes the photovoltaic modules in the array. Default is Standard module
Module Type Options
Type Approximate Efficiency Module Cover Temperature Coefficient of Power
Standard (crystalline Silicon) 15% Glass ‐0.47 %/°C
Premium (crystalline Silicon) 19% Anti‐reflective ‐0.35 %/°C
Thin film 10% Glass ‐0.20 %/°C
Array Tilt (deg):
Photovoltaic array tilt angle for different roof
pitches
Roof Pitch (rise/run) Tilt Angle (deg)
12‐Apr 18.4
12‐May 22.6
12‐Jun 26.6
12‐Jul 30.3
12‐Aug 33.7
12‐Sep 36.9
12‐Oct 39.8
12‐Nov 42.5
12‐Dec 45
Array Type: describes whether PV module are fixed, or whether they move to track the movement of the sun across the sky with one or two axes of rotation
For systems with fixed arrays, you can choose between an open rack or a roof mount option. The open rack option is appropriate for ground‐mounted systems. It assumes
that air flows freely around the array, helping to cool the modules and reduce cell operating temperatures. (The array's output increases as the cell temperature decreases
at a given incident solar irradiance.)
The tilt angle is the angle from horizontal of the photovoltaic modules in the array. For a fixed array, the tilt angle is the angle from horizontal of the array where 0° = horizontal, and 90° = vertical. For arrays with one-axis tracking, the tilt angle is the angle from horizontal of the tracking axis. The tilt angle does not apply to arrays with two-axis tracking.
By default, PVWatts® sets the tilt angle to 20 degrees for a fixed system. If array type is switched to a one axis tracking system, the tilt angle is set to a default of 0 degrees. Often, users set
Array Azimuth (deg):
Heading Azimuth Angle
N 0°
NE 45°
E 90°
SE 135°
S 180°
SW 225°
W 270°
NW 315°
System Losses:
100% × [ 1- ( 1 - 0.02 ) × ( 1 - 0.03 ) ×
( 1 - 0.02 ) × ( 1 - 0.02 ) ×
( 1 - 0.005 ) × ( 1 - 0.015) ×
( 1- 0.01 ) × ( 1 - 0.03) ] = 14%
For a fixed array, the azimuth angle is the angle clockwise from true north
describing the direction that the array faces. An azimuth angle of 180° is for a
The system losses account for performance losses you would expect in a real system that are not explicitly calculated by the PVWatts® model equations.
The default value for the system losses of 14% is based on the categories in the table below, and calculated as follows:
System Loss Categories:
Soiling
Shading
Snow
Mismatch
Wiring
Connections
Light-Induced Degradation
Nameplate Rating
Age
Availability
Invert Efficiency:
DC to AC Size Ratio:
Resistive losses in the DC and AC wires connecting modules, inverters, and other parts of the system. The default value is 2%.
Losses due to dirt and other foreign matter on the surface of the PV module that prevent solar radiation from reaching the cells. Soiling is location‐ and weather‐
dependent. There are greater soiling losses in high‐traffic, high‐pollution areas with infrequent rain. For northern locations, snow reduces the energy produced,
depending on the amount of snow and how long it remains on the PV modules. NREL continues to work on improving the modeling of soiling and snow and is
working to include historical datasets as available.
Reduction in the incident solar radiation from shadows caused by objects near the array such as buildings or trees, or by self‐shading for fixed arrays or arrays with
two‐axis tracking. PVWatts® calculates self‐shading losses for one‐axis trackers, so you should not use the shading loss to account for self‐shading with the one‐axis
tracking option. The default value of 1% represents an array with no shading. Shading analysis tools can determine a loss percentage for shading by nearby objects.
For fixed arrays or arrays with two‐axis tracking that consist of multiple rows of modules, you can use the table below to choose a loss percentage to represent self‐
shading (losses that occur when modules in one row cause shadows on those in an adjacent row). The graph shows the shading derate factor as a function of ground
cover ratio (GCR) for one‐ and two‐axis tracking, and for fixed arrays with tilt angles ranging from 0 to 40 degrees from horizontal. To convert the derate factor to a
percentage, subtract it from one and multiply it by 100%. The GCR is defined as the ratio of the array area to the ground or roof area occupied by the array. The
graph shows that for a given tracking option or tilt angle, a derate factor closer to 1 (less shading loss) corresponds to more space between rows (smaller GCR). For
fixed arrays, you can reduce the area required by the array by using a smaller tilt angle with less row spacing (larger GCR) to achieve the same shading derate factor.
For a given shading derate factor, two‐axis tracking requires the most ground area compared to one‐axis tracking or a fixed array. If you know the GCR value for your
array, you can use the graph to estimate the appropriate shading derate factor. Industry practice is to optimize the use of space by configuring the PV system for a
GCR that corresponds to a shading derate factor of 0.975 (2.5% loss). Shading derate factor versus ground cover ratio (GCR) for different tracking options and tilt
angles
Reduction in the system's annual output due to snow covering the array. The default value is zero, assuming either that there is never snow on the array, or that the
array is kept clear of snow.
Electrical losses due to slight differences caused by manufacturing imperfections between modules in the array that cause the modules to have slightly different
The DC to AC size ratio is the ratio of the inverter's AC rated size to the array's DC rated size. Increasing the ratio increases the
system's output over the year, but also increases the array's cost. The default value is 1.10, which means that a 4 kW system size
would be for an array with a 4 DC kW nameplate size at standard test conditions (STC) and an inverter with a 3.63 AC kW nameplate
size.
Resistive losses in electrical connectors in the system. The default value is 0.5%.Effect of the reduction in the array's power during the first few months of its operation caused by light‐induced degradation of photovoltaic cells. The default value is
1.5%.
The nameplate rating loss accounts for the accuracy of the manufacturer's nameplate rating. Field measurements of the electrical characteristics of photovoltaic
modules in the array may show that they differ from their nameplate rating. A nameplate rating loss of 5% indicates that testing yielded power measurements at
Standard Test Conditions (STC) that were 5% less than the manufacturer's nameplate rating. The default value is 1%.
Effect of weathering of the photovoltaic modules on the array's performance over time. The default value is zero.
Reduction in the system's output cause by scheduled and unscheduled system shutdown for maintenance, grid outages, and other operational factors. The default
value is 3%.
The inverter's nominal rated DC‐to‐AC conversion efficiency, defined as the inverter's rated AC power output divided by its rated DC
power output. The default value is 96%.
Greenhouse Gas Reductions TableSource Metric tons of CO2/year Comments
1. Load shift from water/energy bank 94,000 From GFO‐16‐305 proposal
2. 640 acres of existing solar arrays 70,000 110 MW of existing solar arrays
3. 640 acres of new solar arrays 70,000 110 MW of dual use ponds & arrays
4. GHG created at 0.5 MAF surface reservoir 30,000 From Oct. 2016 BioScience article**
Total 264,000 Equivalent to taking 56000 cars off the road
Background InformationGHG reduction load shift to over generation risk period 173,000 MWh
Heat rate 0.1027 therm/kWh
Emissions factor (CO2e) 0.0053 metric tons/therm
Row 1: Load shift from water/energy bank
Equation
Total GHG reduction from load shift 94,000 metric tons CO2e/year Calculation
Greenhouse Gas Reductions* from Willow Springs Water Bank
173,000MWh
)(.
.
) ≈ 94,000 metric tons CO2e/year
Greenhouse Gas Reductions TableSource Metric tons of CO2/year Comments
1. Load shift from water/energy bank 94,000 From GFO‐16‐305 proposal
2. 640 acres of existing solar arrays 70,000 110 MW of existing solar arrays
3. 640 acres of new solar arrays 70,000 110 MW of dual use ponds & arrays
4. GHG created at 0.5 MAF surface reservoir 30,000 From Oct. 2016 BioScience article**
Total 264,000 Equivalent to taking 56000 cars off the road
PVWatts: Monthly PV Performance Data
Requested Location: Rosamond, CA
Location: LANCASTER GEN WM FOX FIELD, CA
Lat (deg N): 34.73
Long (deg W): 118.22
Elev (m): 713
DC System Size (kW): 110,000
Module Type: Standard
Array Type: 1‐Axis Tracking
Array Tilt (deg): 34.7
Array Azimuth (deg): 150
System Losses: 12.29
Invert Efficiency: 98
DC to AC Size Ratio: 1.3
Ground Coverage Ratio: 0.4
Average Cost of Electricity Purchased from Utility ($/kWh): No utility data available
Capacity Factor (%) 26.0
Month AC System Output(kWh) Solar Radiation (kWh/m^2/day)
Plane of Array Irradiance
(W/m^2)
DC array Output
(kWh)
1 17,314,012 6.21 192.65 17,947,282
2 15,624,778 6.16 172.35 16,219,324
3 21,343,794 7.91 245.10 22,344,628
4 23,046,252 8.81 264.23 24,059,796
5 25,195,132 9.40 291.53 26,003,326
6 24,387,458 9.59 287.75 24,898,106
7 23,772,776 9.05 280.44 24,261,034
8 24,384,544 9.56 296.33 24,880,996
9 21,425,146 8.51 255.39 21,934,544
10 20,185,296 7.49 232.15 20,900,452
11 17,893,428 6.82 204.64 18,434,254
12 16,274,081 5.79 179.40 16,790,358
Total 250,846,697 95.30 2,901.97 258,674,100
National Renewable Energy Laboratory (NREL) PVWatts Calculator is a web application that
estimates the electricity production of a grid‐connected roof‐ or ground‐ mounted photovoltaic
system based on a few inputs. PVWatts calculates estimated values for the system's annual and
monthly electricity production. PVWatts is suitable for very preliminary studies. Website ‐
Background information from PVWatts
Row 2 and 3: 640 acres of solar array GHG emission reductions
Annual total output emission rates for greenhouse gases (GHGs) can be used as default factors for estimating GHG emissions from electricity use when developing a carbon footprint or emissions inventory. Annual non‐baseload output
emission rates should not be used for those purposes, but can be used to estimate GHG emissions reductions from reductions in electricity use.
eGRID2014 GHG Annual Output Emission Rates
Carbon dioxide (CO2) (lb/MWh) Methane (CH4) (lb/GWh) Nitrous oxide Carbon Methane Nitrous
CAMX WECC California 619.9 36.7 4.5 599.8 24.2 2.9
Total DC array Output (kWh) annual 258,674,100 kWh Input NumberNon‐baseload output emission rate 0.27 tons CO2/MWh Input Number
Equation
Total GHG emission reductions from solar arrays 70,000 CalculationMetric tons of CO2/year
eGRID subregion acronym eGRID subregion name
Annual total output emission rates
The term “baseload” refers to those plants that supply electricity to the grid when demand for electricity is low.
Baseloaded plants are usually called upon to provide electricity to the grid no matter what the demand for electricity is during any given period of time, and generally operate except when undergoing routine or unscheduled maintenance.
Non‐baseload emission rates are a slice of the system total mix, with a greater weight given to plants that operate coincident with peak demand for electricity
Source: https://www.epa.gov/sites/production/files/2015‐10/documents/egrid2012_ghgoutputrates_0.pdf
Conversion factor: 1 pound = 4.5359E‐4 metric tons
Convert pounds CO2 to metric tons CO2
Annual non‐baseload output
258,674,100
0.27metrictonsCO2
, ⁄
599.8 .(. ^
.≈ 0.27 metric tons CO2/MWh
Greenhouse Gas Reductions TableSource Metric tons of CO2/year Comments
1. Load shift from water/energy bank 94,000 From GFO‐16‐305 proposal
2. 640 acres of existing solar arrays 70,000 110 MW of existing solar arrays
3. 640 acres of new solar arrays 70,000 110 MW of dual use ponds & arrays
4. GHG created at 0.5 MAF surface reservoir 30,000 From Oct. 2016 BioScience article**
Total 264,000 Equivalent to taking 56000 cars off the road
Assumptions1 km2 = 1.0764X107 ft2
1 Tg = 1,000,000 metric tons
0.5 MAF is 5X105 Acre‐foot
Surface area ‐ 3.10E+05 Known numberAnnual CO2 Equivalents (Tg CO2 Eq per year) ‐ 773.1 Known number
Equation
Convert from km2 to Acre‐foot 1.30E+10 Acre‐foot Calculation
Equation
Convert from Tg CO2/year to metric tons CO2/year 7.73E+08 metric tons CO2/year Calculation
What we know from bio. Science article What we are trying to find Xmetric tons CO2/year
Equation
Row 4: GHG created at 0.5 MAF surface reservoir
mean depth of reservoir 170 feet. Took the average of all reservoirs and dams depth. Source: https://en.wikipedia.org/wiki/List_of_dams_and_reservoirs_in_California
Reservoir surface area 0.31X106 km2 produces 773.1 Tg CO2 equivalence
Source: Greenhouse Gas Emissions from Reservoir Water Surfaces: A New Global Synthesis https://academic.oup.com/bioscience/article/66/11/949/2754271/Greenhouse‐Gas‐Emissions‐from‐
Reservoir‐Water
0.31X10 2(1.0764X10^7 ft2
1 km2 )(170 ft)( ,
) ≈ 1.30X1010 Acre‐foot
773.1 2/, ,
) ≈ 7.73X108 metric tons CO2/year
1.30X10^10 Acre−foot
7.73X10^8 metric tons CO2/year
5X105Acre footmetric tons CO2/year
(Xmetric tons CO2/year)(1.30X10^10 Acre−foot ) = (5X105Acre foot)(7.73X10^8 metric tons CO2/year)
metric tons CO2/year = ( ^ )(7.73X10^8 metric tons CO2/year)
1.30X10^10 Acre−foot
Calculate for metric tons of CO2/year 30,000 metric tons CO2/year Calculation
metric tons CO2/year ≈ 30,000 metric tons CO2/year
Greenhouse Gas Reductions TableSource Metric tons of CO2/year Comments
1. Load shift from water/energy bank 94,000 From GFO‐16‐305 proposal
2. 640 acres of existing solar arrays 70,000 110 MW of existing solar arrays
3. 640 acres of new solar arrays 70,000 110 MW of dual use ponds & arrays
4. GHG created at 0.5 MAF surface reservoir 30,000 From Oct. 2016 BioScience article**
Total 264,000 Equivalent to taking 56000 cars off the road
Equation
Average fuel economy of cars/trucks 21.6 miles/gallon
Average miles traveled 11,346 miles
CO2 emitted per gallon of gas burned 8.89 × 10‐3 metric tons
1 CO2, CH4, and N2O/0.986 CO2
Emissions per vehicles per year (vehicles mile traveled)
Number of cars 56,000 Calculation
Source: https://www.epa.gov/energy/ghg‐equivalencies‐calculator‐calculations‐and‐references
8.89 × 10‐3 metric tons CO2/gallon gasoline × 11,346 VMT car/truck average × 1/21.46 miles per gallon car/truck
average × 1 CO2, CH4, and N2O/0.986 CO2 = 4.73 metric tons CO2E /vehicle/year
Greenhouse Gases EquivalencieTo determine annual greenhouse gas em
vehicle, the following methodology wa
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Gallons of gasoline consumed was m
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emitted per vehicle per year. Carbon dio
then divided by the ratio of carbon diox
vehicle greenhouse gas emissions to
methane and nitrous oxide e
In 2013, the ratio of carbon dioxide emissions to total
greenhouse gas emissions (including carbon dioxide, methane,
and nitrous oxide, all expressed as carbon dioxide equivalents)
for passenger vehicles was 0.986 (EPA 2015).
, /
. / /≈ 56,000 vehicles
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s used: vehicle miles
age gas mileage to
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