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Folie 1

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RWTH Aachen University is running ambitious research projects ... reflection seismics and earthquake seismology. potential field and electromagnetic geophysics ... – PowerPoint PPT presentation

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Title: Folie 1


1
GEOPOT
GEOthermal POwer in Turkey (GEOPOT) Virginie
Harcouet, Christoph Clauser Applied Geophysics
and Geothermal Energy E.ON Energy Research
Center RWTH Aachen University
2
Outline
  • Motivation and vision
  • Targets and synergy with running projects
  • MeProRisk project at RWTH Aachen University
  • Seismic risk assessment
  • Socio-economic issues
  • Final remarks

3
Motivation 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

4
Required 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

5
Institutions
  • 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

6
Turkeys 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.

7
Geology
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

8
Studied 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

9
Geology 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.

10
Hydrogeology
  • 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)

11
Targets 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

12
MeProRisk 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.

13
MeProRisk 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
14
MeProRisk 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
15
MeProRisk 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
16
MeProRisk 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
17
Industry 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

18
Seismic 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.

19
Seismic Risk
  • Micro-seismicity network can be used near the
    geothermal area and new seismological stations
    can be established in the region

20
Socio-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.

21
Public 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.

22
Feasibility 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.

23
Scientific 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.
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