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Proceedings World Geothermal Congress 2020
Reykjavik, Iceland, April 26 – May 2, 2020
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Geothermal Energy Use: Projections and Country Update for Turkey
Orhan Mertoglu1, Sakir Simsek2, and Nilgun Basarir1
1Turkish Geothermal Association, And Sokak 8/2, Çankaya/Ankara
2Hacettepe University UKAM/Beytepe-Ankara
o.mertoglu20@gmail.com
Keywords: Geothermal, potential, country update, Turkey.
ABSTRACT
Turkey has achieved important geothermal developments since 2015. Since the 1960’s, about 460 geothermal fields have been
discovered in Turkey. Geothermal direct-use applications have reached 3828,5 MWt geothermal heating, including district heating
(1120 MWt), 4.5 million m2greenhouse heating (855 MWt), thermal facilities, hotels, etc. heating 435 MWt, balneological use
(1400 MWt), agricultural drying (9.5 MWt) and ground source heat pump applications (8.5 MWt).
Geothermal electricity production installed capacity is 1663 MWe (about 1263 MWe binary cycle and about 400 MWe flash steam
geothermal power plants) as of December 2020. Liquid carbon dioxide and dry ice production factories, and greenhouse heating are
integrated into the Kizildere and Salavatli geothermal power plants. Deep reservoir explorations are ongoing for electricity
production purposes. For this reason, deep drilling targets have reached up to 4800 m. The increase of directional drilling and coil
tubing operations are other important developments for the geothermal fields in Turkey.
The issued geothermal law and incentives contributed to the increase in geothermal electricity production investments within the
Turkish private sector. Besides the hydrothermal system utilization, Turkey shall give emphasis to EGS systems for future
projections. The Turkish Geothermal Association gave emphasis and advice on continuing the feed in tariff, which ended at the end
of 2020 and the Turkish Government decided to be continued additional 10 years with same tarif value.
The total hydrothermal possible theoretical geothermal heat potential is 60,000 MWt, according to heat flow maps, measured well
depth temperatures and calculations made for 4 km depth. Turkey's total geothermal electricity production potential (hydrothermal,
0-4 km) can be estimated as 4500 MWe with existing 10.5 US cents/kWh incentive, and 10 years purchase guarantee. The technical
and economical EGS geothermal electricity production potential has been projected as 20,000 MWe if the 15 US cents/kWh
incentive with minimum 15 year purchase guarantee would be possible.
It is known that CO2in the geothermal fields in Turkey is formed mostly by the marble and carbonate reservoir rocks due to the
effect of the water and heat. CO2is emitting naturally towards the atmosphere at ground surface from the reservoir. It is a natural
discharge of CO2and is independent to the existence of geothermal power plants. For this reason, 50-70 % decrease in the CO2
amount in 10 years in the geothermal fields in Turkey has been obtained, and is ongoing The reasons of the decline are explained in
the paper. As a natural result of CO2decrease in the geothermal fields, the downhole pump usage in the geothermal fields will be
increased. Existing CO2in the geothermal fluid is the advantage for the artesian well flow, but it is a disadvantage for the power
plant electricity generation.
1. INTRODUCTION
The first geothermal research and investigations in Turkey started by MTA (General Directorate of Mineral Research and
Exploration) in the 1960’s (MTA, 2005). Turkey has achieved important geothermal developments in the last 5 years. About 13 %
of Turkey’s geothermal potential is utilized so far in direct use and electricity production.
Today 17 cities are heated partly with geothermal in Turkey. These geothermal district heating systems have been constructed since
1987 and many developments have been achieved in technical and economical aspects. The first geothermal cooling application has
been realized in Izmir - Balcova by Izmir Jeotermal Inc. In 2018, for cooling of 1900 m2indoor area by lithium bromide absorption
and 90/85°C geothermal temperature regime by supplying 6/9 °C clean cold water to the coolers in the buildings. The 2025 target
of Turkey for geothermal direct use, including mainly geothermal heating like district heating, greenhouse heating, thermal
facilities heating and cooling and balneological use, has been estimated as 11.150 MWt.
2. GEOLOGY BACKGROUND
Turkey is geologically divided into three main tectonic units: the Pontides, the Anatolides-Taurides and the Arabian Platform
(Ketin 1966). These terranes were amalgamated during the Alpine orogeny. The relics of the oceans, which once separated these
terranes, are widespread through the Anatolia; they are represented by ophiolite and accretionary mixtures and complexes.
The three terranes, which make up the Pontides, namely the Strandja, Istanbul and Sakarya terranes, have Laurasian affinities. In
contrast to the Pontic terranes, the Anatolide-Tauride terrane has not been affected by the Variscan and Cimmeride deformation and
metamorphism but was strongly shaped by the Alpine orogeny. The Anatolide-Tauride terrane is subdivided into several zones,
mainly on the basis of type and age of Alpine metamorphism. The Southeast Anatolia forms the northernmost extension of the
Arabian Platform and shares many common stratigraphic features with the Anatolide-Tauride terrane. The final amalgamation of
the terranes in the Oligo- Miocene ushered a new tectonic era characterized by continental sedimentation, calc-alkaline magmatism,
Mertoglu et al.
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extension and strike-slip faulting. Most of the present active structures, such as the North Anatolian Fault, and most of the present
landscape are a result of this neotectonic phase (Okay, 2008).
Due to its complex geology and active tectonic properties, Turkey has high geothermal (hydrothermal and EGS) potential
distributed in whole Turkey with different temperature intervals (Figure 1). Due to the effect of extensional tectonism, the western
part of Turkey has the most abundant geothermal activity with highest temperatures (up to 287 °C in Manisa -Alasehir in Gediz
Graben) (Figure 2). Faults accommodating the deep circulation of hydrothermal fluids of mostly meteoric origin are the primary
means by which of geothermal systems are controlled in this region.
In Büyük Menderes Graben located in Aydin - Denizli province, around 1000 MWe geothermal electricity installed capacity exist
which constitutes the majority of total geothermal electricity production of Turkey (Figure 3).
Figure 1: Distribution of geothermal resources and the active faults of Turkey (Simsek, 2020).
3. GEOTHERMAL RESOURCES AND POTENTIAL
3.1. Geothermal Potential of Hydrothermal Systems
The total geothermal theoretical heat potential of Turkey (hydrothermal 0–4 km depth) has been calculated by Turkish Geothermal
Association as 60,000 MWt. The total geothermal electricity technical potential of Turkey (hydrothermal 0–4 km depth) is 4500
MWe. The 2025 target of Turkey is 2500 MWe with incentive (10.5 US cents/kWh feed in tariff, durations of the FIT effectiveness
in 10 years).
3.2. EGS Potential and Projections
We estimated the EGS-Enhanced Geothermal System electricity production technical potential of Turkey (3–5 km depth) as
400,000 MWe. The EGS-Enhanced Geothermal System target of Turkey (3-5 km depth) is 20,000 MWe. This production potential
is expected to be realized with the feed in tariff of 15 US cents/kWh for 15 years purchase guarantee.
The highest reservoir temperature of 287 °C has been measured at 2750 m depth at Manisa-Alasehir geothermal field in Gediz
Graben. A high temperature geothermal field (295°C) at a depth of about 3000 m was also discovered at Nigde province in Central
Anatolia.
Şimşek, 2020
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Figure 2: Main geothermal fields of Western Anatolia (Simsek, 2020).
Şimşek, 2020
Deniz li-Sarayköy Pekdemir
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Figure 3: Geothermal fields of the Büyük Menderes Graben (Simsek, 2020).
4. GEOTHERMAL UTILIZATION
As at the end of December 2020, there exist 62 operating geothermal power plants at 27 geothermal fields in Turkey which have a
total installed capacity of 1663 MWe (Figure 4). Deep reservoir explorations are going on for electricity production purposes. The
increase of directional drillings and coil tubing operation applications are very important for developments of geothermal reservoirs
in Turkey. Deep drilling targets have reached up to 4800 m depth. The successful results have been obtained in deep marble
reservoirs (about 250°C) at Kizildere and Tekkehamam geothermal fields (Simsek, 2017, 2020).
Figure 4: Geothermal electricity production increase in Turkey (Mertoglu et al, 2020).
Şimş ek, 2020
0
200
400
600
800
1000
1200
1400
1600
1800
1986
2000
2005
2010
2014
2016
Dec. 2020
MWe Install Power
Year
20 MWe
20 MWe
20 MWe
82 MWe
400 MWe
721 MWe
1663 MWe
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The operational capacities of the city based geothermal district heating systems (GHDS) existing in Turkey are as follows: Gönen
(Commissioned: 1987, 3,400 residences), Simav (1991, 14,500 residences), Kirsehir (1994, 1,900 residences), Kizilcahamam
(1995, 2,500 residences), Izmir (1996, 37,000 residences), Sandikli (1998, 11,000 residences), Afyon (1996, 30,000 residences),
Kozakli (1996, 3,000 residences), Diyadin (1999, 570 residences), Salihli (2002, 7,500 residences), Edremit (2003, 5,500
residences), Balikesir-Bigadic (2005, 1,500 residences), Yozgat-Sorgun (2008, 1,500 residences), Izmir-Bergama (450 residences),
Izmir- Dikili (2000 residences), Denizli-Saraykoy (2,500 residences) and Balikesir-Sindirgi (2014, 300/3000 residences). Today, as
low as 40-45°C temperature geothermal waters are also used for space heating in Turkey without heat pumps (Mertoglu et al,
2020).
Some of the existing cities heating have increased their heating capacities as it can be seen in Table 1. Geothermal greenhouse
heating applications have reached 4,5 million m2during last five years. Ground source heat pump (GSHP) applications in Turkey
started in 2000’s for residential single family houses with a total installed capacity of 586 kWt. Today, 90 GSHP applications are
closed systems with installed capacity of 8,5 MWt (Mertoglu et al. 2020). In recent years, as a new source waste heat from
balneological use is recovered.
Table 1: Geothermal utilization capacities in Turkey
4. DISCUSSION AND CONCLUSIONS
About 460 geothermal fields have been discovered in Turkey. Rapid development at geothermal electricity installed capacity
reached up to 1663 MWe as of December 2020. The capacity has increased more than twice since 2016.
Geothermal direct-use applications have reached 3828,5 MWt geothermal heating, including district heating (1120 MWt), 4,5
million m2greenhouse heating (855 MWt), thermal facilities, hotels, etc. heating 435 MWt, balneological use (1400 MWt),
agricultural drying (9,5 MWt), geothermal cooling (0,35 MWt) and Groundsource Heat Pump applications (8,5 MWt). Deep
reservoir explorations are ongoing for electricity production purposes. For this reason, deep drilling targets have reached up to
4500m. Successful results have been obtained for the exploration of deep reservoirs. As natural result of CO2decrease in the
geothermal fields; The downhole pump usage in the geothermal fields will be increased in coming years.
The increase of directional drillings and coil tubing operation applications are other important environmental and economic
developments for the geothermal fields in Turkey. The EGS-Enhanced Geothermal System target of Turkey (3-5 km) is 20.000
MWe. This production potential expected to be realized during the next 20 years. Heat pump (HP) applications in Turkey started in
2000’s and with increasing interest in renewables, number of HP systems has reached to 149 with a total installed capacity of 120
MWt as of December 2019. The 2025 target of Turkey about geothermal direct use has been estimated as 11.150 MWt.
UTILIZATION
CAPACITY
GEOTHERMAL DISTRICT HEATING
(CITY, RESIDENCES)
126.000 RESIDENCES EQUIVALENCE
(1120 MWt)
GREENHOUSE HEATING
4,5 Million m2(855 MWt)
HEATING OF THERMAL FACILITIES, SPAS,
THERMAL HOTELS AND TIME SHARE FACILITIES
48.60 0 residences equivalence
(435 MWt)
HEAT ENERGY OF THERMAL WATER USE IN
HOTELS, SPAS AND AND TIME SHARE
FACILITIES
520 GEOTHERMAL SPA
(1400 MWt) (about 23 Million guests/annual)
AGRICULTURAL DRYING
9,5 MWt
GEOTHERMAL COOLING
0,35 MWt
HEAT PUMPS; GSHP
120 MWt; 8,5 MWt
TOTAL HEAT USE
3828,5 MWt
(373.000 Residences Equivalence)
TOTAL ELECTRICTY PRODUCTION
1663 MWe
(Aydın, Denizli, Manisa, Çanakkale, Afyon)
CARBONDIOXITE PRODUCTION (Food grade
Liquid CO2)
400.000 Tons/year
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REFERENCES
Geothermal Energy Development Report, Turkish Geothermal Association (TGA-TJD), 2020. Ankara.
Ketin I., Türkiye Jeolojisine Genel bir Bakış, İstanbul Teknik Üniversitesi, 1983.
Mertoglu, O., personal communication, 2020
Mertoglu, O., Basarir, N., Geothermal District Heating and Power Generation Experience in Turkey, EGW 2018, Strasbourg.
Mertoglu, O., Simsek, S.,Basarir, N., Paksoy.H., Country Update report. European Geothermal Congress, EGC 2019, The Haague,
Netherland.
MTA (General Directorate of Mineral Research and Exploration of Turkey) Geothermal Inventory of Turkey, MTA publication,
2005, Ankara.
Okay A., Geology of Turkey: A Synopsis, Anschnitt, 21, 19-42, 2008.
Simsek, S., The figure of Main Geothermal Fields of Western Anatolia, 2020.
Simsek, S., The Turkish Geothermal Experience, Chapter 5 Book of Perspectives for Geothermal Energy in Europe (Edited by:
Ruggero Bertani- Enel Green Power, Italy) p: 157-186, http: //www.worldscientific.com/ worldscibooks/10.1142/q0069,
ISBN: 978-1-78634-231-7. World Scientific Publishing Co Pte Ltd. London WC2H 9HE. 2017.