Title: Folie 1
1GEOPOT
GEOthermal POwer in Turkey (GEOPOT) Virginie
Harcouet, Christoph Clauser Applied Geophysics
and Geothermal Energy E.ON Energy Research
Center RWTH Aachen University
2Outline
- Motivation and vision
- Targets and synergy with running projects
- MeProRisk project at RWTH Aachen University
- Seismic risk assessment
- Socio-economic issues
- Final remarks
3Motivation and vision
- Turkey has a large unused potential for the
production of geothermal power and heat - RWTH Aachen University is running ambitious
research projects to improve the exploration,
development, and operation of geothermal fields - ZORLU Energy expressed interest to be an
industrial partner in a EU demonstration project - In FP7 we are expecting a call concerning
- Increased electricity production from
low/medium enthalpy geothermal sources
4Required expertise
- geology
- reflection seismics and earthquake seismology
- potential field and electromagnetic geophysics
- petrophysics and borehole geophysics
- geothermics
- computational engineering science
- drilling technology
- power conversion technology
- (smart) grid design
- economics
- operation and maintenance
- public outreach
5Institutions
- BRGM
- E.ON
- CAPD
- CNR-IGG
- Geophysica
- Marmara Research Centre
- RWTH-E.ON ERC
- RWTH-IFHT (Institute for High Voltage Technology)
- RWTH-IDG (Institute of Steam and Gas turbines)
- ZORLU
- Eventual additional institute GFZ Potsdam
6Turkeys geothermal potential
- Turkeys rich geothermal resources are used only
to a small degree for the generation of the
countrys electric energy needs. - It is a promising country to develop, test, and
apply new methodology for the exploration,
development, and operation of geothermal
low/medium-enthalpy reservoirs. - ?However the conversion of geothermal energy into
electric energy is associated with uncertainty
and risk.
7Geology
Simav graben formed by NW-SE trending and
north-dipping faults the latest products of the
N-S extensional tectonics
- Turkey is located within the Alpine Himalayan
orogenic belt - Western Anatolia is a tectonically active region
presence of large grabens
8Studied area Simav (Kütahya) Geothermal Field
- Simav Geothermal fluids are used for
- District heating capacity of 66 MWt
- The largest geothermal district heating system in
Turkey - Deep geothermal wells located 4 km North of Simav
(720 m deep, 163 C and 70 l/s) - Balneology
- greenhouses
9Geology Simav
- Basement Paleozoic Menderes Massif rocks
- Main rocks are overlain by Mesozoic Kirkbucak
formation and Cenozoic Toklargozu and Eynal
formations. - Nasa basalts are the youngest volcanics in the
region.
10Hydrogeology
- Reservoir rocks
- - Mesozoic Kirkbucak formation (especially
marbles)? fractures and faults. - - Nasa basalts ? fractures.
- Cap rock in the geothermal system Imperable
Neogene rocks (such as claystone)
11Targets and synergy with running projects
- Our project (GEOPOT) will apply, in the region of
Simav (Turkey), techniques developed in the
parallel method-oriented MeProRisk project (RWTH,
Aachen) in order to - explore and develop a geothermal field in Turkey
- quantify data uncertainty and corresponding
economic risk - Quantify seismic risk due to the operation of a
geothermal field - Construct a demonstration size (5 MW 20 MW),
modular geothermal power plant
12MeProRisk Description of the multi-stage strategy
- This project is based on (1) a novel multi-stage
strategy for the exploration of geothermal
reservoirs and (2) prognostic simulation tools
with risk assessment capabilities for the
development and operation of geothermal
reservoirs. - The strategy consists of a combination of surface
and borehole geophysics, petrophysics, geology,
and numerical simulation technology. - Simulations are performed on a hierarchy of
models for flow and transport which differ in
complexity and data quality.
13MeProRisk project at RWTH Aachen University
Basic information Geology
Development Production
Exploration
a
Geophysics Surface borehole Lab
Model concept Numerical code
b
c
Exploration layout
Production -Monitoring -Flow tests
Inversion Model update calibration
h
f
d
Evaluation -Risk -Scenarios -Planning
Uncertainty Resolution Sensitivity
g
e
14MeProRisk project Exploration phase
a based on available a priori information.
Initial zero-generation model
Basic information Geology
a
Geophysics Surface borehole Lab
Model concept Numerical code
c/d Then a combination of forward and inverse
simulations is performed.
b
c
Exploration layout
? e/f Optimization of location, depth, and
number of exploration boreholes and quantify the
uncertainty of the models predictions.
Inversion Model update calibration
f
d
Uncertainty Resolution Sensitivity
Information from these boreholes is then used to
generate the first-generation model.
e
15MeProRisk project Exploration phase
Basic information Geology
First-generation model
a based on the information from boreholes.
a
Geophysics Surface borehole Lab
Model concept Numerical code
b
c/d Simulations based on this model are tested
against independent data from existing boreholes.
c
Exploration layout
Inversion Model update calibration
? e/f Calibrated version of the model is used
again to optimize location, depth, and number of
additional exploration boreholes.
f
d
Uncertainty Resolution Sensitivity
Information from these boreholes is then used to
generate the second-generation model.
e
16MeProRisk project Exploration phase
Basic information Geology
a
Geophysics Surface borehole Lab
This process is iterated until a model is
obtained with sufficiently high prognostic
probability to optimize location, depth, and
number of production and injection boreholes for
the reservoir to be developed.
Model concept Numerical code
b
c
Exploration layout
Inversion Model update calibration
f
d
Uncertainty Resolution Sensitivity
e
17Industry involvement
- Essential for this demonstration project!
- Commitments required for both
- direct financial contributions (for boreholes,
and surface installations for energy conversion
and transmission) - provision of legal rights and claims for
geothermal fields - As project progresses from research and
exploration towards the installation of a
geothermal power plant, leadership will transfer
from science to industry
18Seismic risk assessment
- Simavs geothermal reservoirs are located in a
tectonically active area where seismicity is to
be expected even without operation of a
geothermal plant. - In addition, reinjection may trigger seismicity.
- ? Quantification of the seismic risk which is
inherent to the development and operation of the
geothermal reservoir. - ?Quantification of the level of ground tremors
which would present a serious disturbance or
threat to the local population and which has to
be avoided.
19Seismic Risk
- Micro-seismicity network can be used near the
geothermal area and new seismological stations
can be established in the region
20Socio-economic issues and public acceptance
- The population of Simav already benefits from
geothermal energy as the district heating system
is the largest in Turkey, still it needs to be
convinced of the benefit derived from a local
production of electric energy. - The 3D reservoir model simulations will be used
to optimize and guarantee the simultaneous
production of electric energy and heat for space
heating.
21Public participation district heating
- Autofinance system 60 of the investment ?The
citizens pay the geothermal heating cost two
years in advance and receive free heat for three
years. - The remaining 40 of the system is supported by
government . - The project payback period is 6 years.
22Feasibility study
- Kose (2007) studied the potential and utilization
of the existing geothermal energy resources in
KutahyaSimav region. - Study of electrical energy generation by a
binary-cycle - Potential of KutahyaSimav geothermal power
plant 2.9 MWe energy (at least 17,020 MWh/yr
electrical energy). - Conclusion the feasibility study indicates that
the project approach is applicable and
economically feasible.
23Scientific benefits
- Development and verification of a unified
exploration, production, and development
technology with prognostic and risk assessment
capability for geothermal steam reservoirs. - Significant extension of current approaches will
enable a much better and quantitative judgment of
the scientific and technological uncertainties
and financial and environmental risks involved.