Alexey V. Kiryukhin1

Leonid K. Moskalev2

1 -Institute of Volcanology and Seismology FEB RAS 2 -SC “Geotherm”

OUTLINE:

V-Mutnovsky Site: 12 MWe PP put in operation since 1999

Mutnovsky Geothermal Field Introduction

Dachny Site: 50 MWe PP put in operation since 2002

History of exploitation:

V-Mutnovsky Site: 12 MWe PP put in operation since 1999

Dachny Site: 50 MWe PP put inoperation since 2002

Mutnovsky Geothermal Field Introduction

Mutnovsky area include magmaticsystem of the active Mutnovsky volcano,numerios steam fields and hot springs

History of exploitation:

V-Mutnovsky Site: 12 MWe PP put in operation since 1999

Dachny Site: 50 MWe PP put inoperation since 2002

Mutnovsky Geothermal Field Introduction

Mutnovsky area include magmaticsystem of the active Mutnovsky volcano,numerios steam fields and hot springs

Mutnovsky is a fracture type geothermalfield:Main and North-East single-faulttype zones include Dachny and V-Mutnovskyproduction reservoirs (Kiryukhin et al, 1998).

Streamlines of fluids from Mutnovsky volcano recharge area to discharge areas through deeper part of zone, where heat and massmagmatic component exchange took place. Main Production Zone shown as a polygon area.

Steam fields: 1 – Active crater of Mutnovsky volcano, 2 – Bottom Field,3 – North Mutnovsky (W), 4 – Dachny;

Hot springs: 5 – Piratovsky, 6 – Verkhne-Zhirovsky.

Conceptual Hydrogeological Model (Recharge\Discharge Conditions)

Conceptual Hydrogeological Model (Geometry of Production Zone)

“Single fault” nature of the Main Production Zone demonstrated by small deviations of the points of the production () and full circulation loss () from plane equation formula Z = -1.691076246561*Х +0.48880109651512*Y +65583.1 Filled symbols correspond to production wells.

Conceptual Hydrogeological Model (Geometry of Production Zone)

Wells isolated from “Single fault” in Dachny Site show low productivity

Conceptual hydrogeological model of the Dachny site Mutnovsky geothermal field was verified based on

Dachny SiteConceptual Hydrogeological Model

•circulation losses and production zones distribution data,•mapping of active fracture zones, •gas and fluid chemistry data, •secondary minerals distributions,•recent results of drilling,•geothermal analog data

Central part of the Dachny represent a “single fault”type geothermal reservoir. Upflow of the high temperature fluids occur in the south-east partof this zone

Numerical Model Setup

In October 2002 Mutnovsky 50 MWe PP was put into operation in Dachny site. The problem of steam supply shortage (60%) to Mutnovsky 50 MWe PP (Dachny) trigged the new reservoir model study.

Basic Software used: TOUGH2V2.0, A-Mesh, HOLA,additional subroutines implementedto model complexreservoir geometry,Graphics software.

3D Grid Generation

3D numerical grid correspond to the fault type geothermal reservoir of the Main Production Zone (120 m thick) connected with the 5-layers array of the Host Rocks.

Numerical Model Setup

Numerical Model Setup

Counters correspond to the top of the Main Production Zone.

Open circles - sources assigned in the model(total upflow recharge estimated 54 kg/s,1390 kJ/kg) Squares – inactive boundary elements (P,T=const) natural state steam discharge.

Crossed squares- inactive boundary elements(P,T=const) liquid discharge.

Sinks/Sources, Boundary Conditions

Numerical Model Setup

Model domains properties based on model calibration

Model Calibration

Temperature Matches: 1 - key elements data 2 – modeling results

Natural State

Model Calibration

Pressure Matches: 1 - key elements data 2 – modeling results

Natural State

Natural State Modeling Output

Temperatures & Flows Distributions Temperatures & Pressure Distributions.

Well Head Pressures (WHP, bars, i) in exploitation wells (SC “Geotherm” data)

Model Calibration

Based on 2002-2004 exploitation data

Mutnovsky PP electricity output, total steam, total separate water production, and separator pressure (bars, i) (SC “Geotherm” data). Note: individual wells parameters data not available.

Model Calibration

Based on 2002-2004 exploitation data

Exploitation wells assigned in the model based on TOUGH2V2.0 coupled wellbore flow option.

Productivity indexes PI0 of five production

wells estimated accordingly to initial exploitation data (rate Q, wellhead pressures WHP) andflowing enthalpies h, reservoir pressure Pr,

bottomhole Pb pressures tables, relative

permeabilities (krs, krw) derived from the

model (TOUGH2 or HOLA).

Model Calibration

Three possible scenarios of additionalrecharge into the Main Production Zoneunder exploitation conditions(including up-flow and reinjection)were tested in the model:

(1) No additional recharge(2) Marginal recharge(3) Downflow recharge

Model Calibration

Best model match (scenario #3, downflow recharge): modeling steam and separate production from wells 016, 26, Е4, 029W, Е5 ( at 5.2 bar i separation pressure) against total production (dots).

Model Calibration

Based on 2002-2004exploitation data

Modeling of Exploitation

Analysis of additional exploitation wells drilling in the high temperature upflow zone and reinjection to maintain sustainable production for 50 MWe Power Plant.

Scenario #1 (no additional recharge): sustainable steam production (96.3 kg/s or 48.2 MWe) during 10-year exploitation period.

Modeling of Exploitation

Scenario #2 (marginal recharge): sustainable steam production (116.7 kg/s or 58.4 MWe) during 10-year exploitation period.

Modeling of Exploitation

Scenario #3 (downflow recharge): sustainable steam production (86.7 kg/s or 43.4 MWe) during 10-year exploitation period.

Modeling of Exploitation

Influence of reinjection on sustainable steam production (based on model scenario #1): 1 - no reinjection, 2 - reinjection 150 kg/s (North Reinjection Site), 3- reinjection 150 kg/s (South Reinjection Site). Upper graphs - total production rates, lower graphs - steam production at 7 bars.

Modeling of Exploitation (20 years)

Conclusions:

Acknowledgements: