Preliminary geological, geochemical and numerical study on the first EGS project in Turkey

Geothermal energy is attracting more and more attention due to its large capacity and lack of dependency on the weather. Currently, many countries have planned enhanced geothermal system (EGS) projects. In this paper the first EGS project in Turkey, which is being implemented at the license area of SDS Energy Inc., in Dikili of the İzmir province, is introduced. Extensive geological, paleostress (279 fault-slip data from 33 locations), geophysical (magnetotelluric and vertical electrical sounding at 80 and 129 locations, respectively) and geochemical studies as well as paleostress measurements have been conducted in this area within the scope of this project. In the light of all these studies, it has been determined that the Dikili region is remarkable in terms of its high thermal gradient of about 7 °C/100 m. The geothermal reservoir formation “the Kozak granodiorite” is a homogeneous, crystalline volcanic rock mass with high radiogenic heat production, and suitable for an EGS application. The analysis shows that the dominating fault system is normal, and the corresponding primary stress regime is extensional. Based on the geological, geophysical surveys and the estimated in situ stresses, numerical studies were carried out to assess the results of the hydraulic fracturing and geothermal energy production using the numerical codes FLAC3Dplus and TOUGH2MP, respectively, in the area A of the Dikili site. The simulation results show that the stimulated reservoir volume and area could reach 44.5 million m3 and 1 km2, respectively, with an injection volume of 122,931 m3. Assuming the fractured zone has a height of 1000 m and a half-length of 1200 m (the distance between injection and production wells being 1000 m), an average overall geothermal capacity of 83.7 MWth in 20 years could be reached with an injection rate of 250 l/s. The injection strategy and design parameters of the reservoir stimulation and geothermal production will be further optimized with the project running.

[1]  J. Angelier,et al.  Tectonic analysis of fault slip data sets , 1984 .

[2]  Thomas Reinsch,et al.  Thermal, mechanical and chemical influences on the performance of optical fibres for distributed temperature sensing in a hot geothermal well , 2013, Environmental Earth Sciences.

[3]  Karsten Pruess,et al.  User's Guide for TOUGH2-MP - A Massively Parallel Version of the TOUGH2 Code , 2008 .

[4]  M. Kühn Reactive Flow Modeling of Hydrothermal Systems , 2013 .

[5]  M. Bozcu,et al.  When Did the Western Anatolian Grabens Begin to Develop? , 2000, Geological Society, London, Special Publications.

[6]  P. T. Branagan,et al.  In Situ Stress and Moduli: Comparison of Values Derived from Multiple Techniques , 1998 .

[7]  Yang Gou,et al.  Investigation of a new HDR system with horizontal wells and multiple fractures using the coupled wellbore–reservoir simulator TOUGH2MP-WELL/EOS3 , 2015, Environmental Earth Sciences.

[8]  J. Angelier,et al.  Inversion of field data in fault tectonics to obtain the regional stress—III. A new rapid direct inversion method by analytical means , 1990 .

[9]  Wang Jiyang,et al.  A Roadmap to Geothermal Energy Development in China , 2012 .

[10]  A. Etchecopar,et al.  An inverse problem in microtectonics for the determination stress tensors from fault striation analysis , 1981 .

[11]  Sadiq J. Zarrouk,et al.  Numerical model of the Habanero geothermal reservoir, Australia , 2015 .

[12]  Albert Genter,et al.  Contribution of the exploration of deep crystalline fractured reservoir of Soultz to the knowledge of enhanced geothermal systems (EGS) , 2010 .

[13]  Fault-slip analysis and paleostress reconstruction , 2011 .

[14]  Michael Kühn,et al.  1 General Significance of Geochemical Models of Hydrothermal Systems , 2004 .

[15]  Tsutomu Yamaguchi,et al.  The Hijiori Hot Dry Rock test site, Japan: Evaluation and optimization of heat extraction from a two-layered reservoir , 2008 .

[16]  R. Armijo,et al.  The inverse problem in microtectonics and the separation of tectonic phases , 1982 .

[17]  D. Schmitt,et al.  An integrative geothermal resource assessment study for the siliciclastic Granite Wash Unit, northwestern Alberta (Canada) , 2014, Environmental Earth Sciences.

[18]  Atsushi Yamaji,et al.  The multiple inverse method: a new technique to separate stresses from heterogeneous fault-slip data , 2000 .

[19]  M. Scheck‐Wenderoth,et al.  Controls on the deep thermal field: implications from 3-D numerical simulations for the geothermal research site Groß Schönebeck , 2013, Environmental Earth Sciences.

[20]  Olaf Kolditz,et al.  Geothermal energy systems: research perspective for domestic energy provision , 2013, Environmental Earth Sciences.

[21]  E. M. Anderson The dynamics of faulting , 1905, Transactions of the Edinburgh Geological Society.

[22]  Olaf Kolditz,et al.  Application of the geomechanical facies approach and comparison of exploration and evaluation methods used at Soultz-sous-Forêts (France) and Spa Urach (Germany) geothermal sites , 2010 .

[23]  David V. Duchane,et al.  Scientific progress on the Fenton Hill HDR project since 1983 , 1998 .