sustainability considerations in the design of big dams: merowe, nile basin
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Sustainability Considerations in the Design of Big Dams: Merowe, Nile Basin. Mentor: Prof. El Fatih Eltahir Group: Anthony Paris, Teresa Yamana, Suzanne Young. Outline. Introduction and motivation Nile hydrology The model Climate Sedimentation Public health - PowerPoint PPT PresentationTRANSCRIPT
Sustainability Considerations Sustainability Considerations in the Design of Big Dams:in the Design of Big Dams:
Merowe, Nile BasinMerowe, Nile Basin
Mentor: Prof. El Fatih EltahirMentor: Prof. El Fatih EltahirGroup: Anthony Paris, Teresa Yamana, Group: Anthony Paris, Teresa Yamana,
Suzanne YoungSuzanne Young
OutlineOutline Introduction and motivationIntroduction and motivation Nile hydrologyNile hydrology The modelThe model ClimateClimate SedimentationSedimentation Public healthPublic health Difficulties and lessons learnedDifficulties and lessons learned ConclusionsConclusions
Goals and MotivationGoals and Motivation Simulate the role of environmental Simulate the role of environmental
engineers in large scale projectsengineers in large scale projects Analyze the effect the Dam will have on Analyze the effect the Dam will have on
the environment and local population, the environment and local population, and make recommendations to mitigate and make recommendations to mitigate effectseffects
Assess whether long-term effects will Assess whether long-term effects will significantly decrease Dam’s lifetime and significantly decrease Dam’s lifetime and plan accordinglyplan accordingly
IntroductionIntroduction Sudan needs EnergySudan needs Energy
19-year old Civil War19-year old Civil War Frequent power blackoutsFrequent power blackouts
Merowe DamMerowe Dam Utilizing HydropowerUtilizing Hydropower
Dam Design DetailsDam Design Details Ten turbines – 1,250 MW CapacityTen turbines – 1,250 MW Capacity Length: 10 kmLength: 10 km Height: 65 mHeight: 65 m Reservoir Length: 170 km Reservoir Length: 170 km
General LayoutGeneral Layout
Average Longterm Monthly Nile flows, 1872-1986
0
5
10
15
20
25
January February March April May June July August September October November December
Dis
char
ge (k
m^3
/mon
th)
Nile discharge, 1872-1986
40
50
60
70
80
90
100
110
120
130
1870 1880 1890 1900 1910 1920 1930 1940 1950 1960 1970 1980
Ann
ual d
isch
arge
(km
^3/y
ear)
Longterm annual average = 88.1 km^3/year
Storage to Elevation RelationshipStorage to Elevation RelationshipReservoir Characteristics
260
270
280
290
300
310
320
330
340
350
0 1E+09 2E+09 3E+09 4E+09 5E+09 6E+09 7E+09
Surface Area (m^2)
Elev
atio
n (m
)
Reservoir Characteristics
260
270
280
290
300
310
320
330
340
350
0 2E+10 4E+10 6E+10 8E+10 1E+11 1.2E+11 1.4E+11
Storage (m^3)
Elev
atio
n (m
)
““The Model”The Model”
The Effect of Climate Change on Dam The Effect of Climate Change on Dam PerformancePerformance
Suzanne YoungSuzanne Young
ClimateClimate
How do changes in river flow caused by How do changes in river flow caused by climate change affect the Merowe Dam’s climate change affect the Merowe Dam’s power capacity?power capacity?
The Big PictureThe Big Picture Documented changes in chemical composition Documented changes in chemical composition
of atmosphere (e.g. COof atmosphere (e.g. CO22 is rising) is rising) Scientists predict if this activity continues, it will Scientists predict if this activity continues, it will
impact the environmentimpact the environment Lots of studies on climate change and global Lots of studies on climate change and global
warming done by governments in U.S., Europewarming done by governments in U.S., Europe Models agree global temperatures will rise, less Models agree global temperatures will rise, less
certain about regional impacts (precipitation)certain about regional impacts (precipitation) We don’t know what is going to happen to Nile We don’t know what is going to happen to Nile
flows!flows!
Range of discharges for major points along the NileRange of discharges for major points along the Nile (Summary of Yates 1998b results)(Summary of Yates 1998b results)
Two numbers on ends of each line represent extreme discharges of six GCM scenarios, whereas boxed number is historic average; Additional tick marks on each line are remaining GCM scenarios, which indicate range of climate change induced flows of Nile Basin.
TO DOTO DO Show different results of studies, and Show different results of studies, and
convince audience that we don’t know convince audience that we don’t know what will happen = document uncertainty!what will happen = document uncertainty!
Calculate hydropower under different Calculate hydropower under different scenarios of climate change:scenarios of climate change: Last 100 yearsLast 100 years Wetter climateWetter climate Drier climateDrier climate
Make recommendations to dam designMake recommendations to dam design
Potential HydropowerPotential Hydropower
Power = γQhγ = ρg
ρ = density of water = 1000 [kg/m3]g = gravity = 9.8 [m/s2]Q = flow at dam [m3/s] h = drop in head between intake to powerhouse and outlet to
river [m]
Sedimentation into the ReservoirSedimentation into the Reservoir
Anthony ParisAnthony Paris
Erosion: Sources of Erosion: Sources of Nile SedimentsNile Sediments
Ethiopian Highlands Ethiopian Highlands (~90%)(~90%)
Travels through the Travels through the Blue Nile and AtbaraBlue Nile and Atbara
The sediment load is The sediment load is most significant most significant during flood season during flood season (July-Oct.)(July-Oct.)
~140 million tones per ~140 million tones per yearyear
TransportationTransportation Suspended LoadSuspended Load
particulates that travel particulates that travel while suspended in the while suspended in the water columnwater column
Distribution:Distribution: 30% Clay (<0.002 mm)30% Clay (<0.002 mm) 40% Silt (0.002-0.02 mm)40% Silt (0.002-0.02 mm) 30% Fine Sand (0.02-0.2 30% Fine Sand (0.02-0.2
mm)mm) High level of total High level of total
suspensionsuspension
Reservoir Reservoir Deposition IDeposition I
When river flow enters a reservoir, its velocity When river flow enters a reservoir, its velocity and transport capacity is reduced and its and transport capacity is reduced and its sediment load is deposited.sediment load is deposited.
The depositional pattern usually starts with The depositional pattern usually starts with coarser material depositing first followed by the coarser material depositing first followed by the fine creating a delta.fine creating a delta.
FactorsFactors Detention TimeDetention Time Shape of reservoirShape of reservoir Operating proceduresOperating procedures
Reservoir Reservoir Deposition IIDeposition II
Hand CalculationsHand Calculations
Calculating QCalculating QSS (“Flow” of Sediments) from Q (“Flow” of Sediments) from Q (Flow)(Flow)
Find Hydrograph with corresponding Sediment Find Hydrograph with corresponding Sediment Load ConcentrationsLoad Concentrations
Convert Load from concentration (mg/L)to Convert Load from concentration (mg/L)to volume (mvolume (m33))
Do linear regression to determine correlation Do linear regression to determine correlation between Qbetween QSS and Q; breaking the hydrograph into and Q; breaking the hydrograph into two sections, monsoon, and non-monsoon.two sections, monsoon, and non-monsoon.
Extrapolate over 100 year monthly data set to Extrapolate over 100 year monthly data set to have Qhave QSS
Hand CalculationsHand Calculations
Calculating Trapping Efficiency – 1st RoundCalculating Trapping Efficiency – 1st Round Brune’s CurveBrune’s Curve C = CapacityC = Capacity I = InflowI = Inflow
TIC
The Effect of the Dam on Public HealthThe Effect of the Dam on Public Health
Teresa YamanaTeresa Yamana
Dams’ Threat to Public HealthDams’ Threat to Public Health
Stagnant water in reservoirs and irrigation Stagnant water in reservoirs and irrigation ditches provide habitat for vectorsditches provide habitat for vectors
Constant supply of water - Dry season no Constant supply of water - Dry season no longer limits vectors longer limits vectors
Merowe Dam expected to increase Merowe Dam expected to increase incidence of Malaria, Schistosomiasis, incidence of Malaria, Schistosomiasis, River Blindness and Rift Valley FeverRiver Blindness and Rift Valley Fever
Malaria TransmissionMalaria Transmission Protozoa Protozoa PlasmodiumPlasmodium
transmitted by Anopheles transmitted by Anopheles mosquitoesmosquitoes
Causes 1 million deaths per Causes 1 million deaths per yearyear
Fever-like symptomsFever-like symptoms A. funestusA. funestus breeds in illuminated breeds in illuminated
shoreline throughout the yearshoreline throughout the year A. gambiaeA. gambiae breeds in reservoir breeds in reservoir
drawdown area in dry season drawdown area in dry season (November – June)(November – June)
Drawdown Area: 2.46 x 108 m3
Drawdown Area: 2.46 x 108 m3
RecommendationsRecommendations
Malaria – Whenever possible, relocate Malaria – Whenever possible, relocate communities outside of mosquito flight communities outside of mosquito flight rangerange
River Blindness – Stop flow over spillways River Blindness – Stop flow over spillways for two days every two weeks over wet for two days every two weeks over wet season to inhibit blackfly breedingseason to inhibit blackfly breeding
More to come (hopefully)More to come (hopefully)
Difficulties Difficulties
TOO BROADTOO BROAD Model is stupidModel is stupid Conflicting expectationsConflicting expectations
ConclusionsConclusions
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