Characterization and Comparison of geothermal fluids geochemistry within the Kizildere Geothermal Field in Turkey: New findings with power capacity expanding studies

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dc.authoridHAKLIDIR, FUSUN SERVIN TUT/0000-0002-9469-8870|aydin, hakki/0000-0001-5653-0121
dc.authorwosidHAKLIDIR, FUSUN SERVIN TUT/ABI-3978-2020
dc.authorwosidaydin, hakki/ABH-2869-2022
dc.contributor.authorHaklidir, Fusun S. Tut
dc.contributor.authorSengun, Raziye
dc.contributor.authorAydin, Hakki
dc.date.accessioned2024-07-18T20:42:43Z
dc.date.available2024-07-18T20:42:43Z
dc.date.issued2021
dc.departmentİstanbul Bilgi Üniversitesien_US
dc.description.abstractThe Kizildere geothermal field is the first known high-temperature geothermal field in Turkey. The field is located in the Buyuk Menderes Graben (BMG), Western Anatolia (Turkey). There are four production sections (reservoir-I, II, III, and IV) with different rock compositions and geochemical characteristics in the production area. Identifying and characterizing these production units may give a good insight into field development plans for a sustainable production. This study aims to characterize production sections of the Kizildere geothermal field using geology, hydrogeochemical properties such as chemistry, stable isotope, and non-condensable gas compositions. The results of gas and water analysis showed that geothermal fluids are of a meteoric origin in all producing sections. It was also found from the analyses that more intensive water-rock interactions take place as the reservoir temperature irises. Based on the different geochemical characteristics of each producing section, we thought that impermeable sediments like mica-schists and chlorite-schists lying between the reservoir units act as a seal. In light of this study, it can be concluded that the Kizildere geothermal reservoir is very heterogeneous due to vertically compartmentalized reservoir sections that require a unique injection-production configuration for a sustainable production lifetime.en_US
dc.identifier.doi10.1016/j.geothermics.2021.102110
dc.identifier.issn0375-6505
dc.identifier.issn1879-3576
dc.identifier.scopus2-s2.0-85103968493en_US
dc.identifier.scopusqualityQ1en_US
dc.identifier.urihttps://doi.org/10.1016/j.geothermics.2021.102110
dc.identifier.urihttps://hdl.handle.net/11411/7380
dc.identifier.volume94en_US
dc.identifier.wosWOS:000661080200004en_US
dc.identifier.wosqualityQ1en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherPergamon-Elsevier Science Ltden_US
dc.relation.ispartofGeothermicsen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectGeochemistryen_US
dc.subjectGeothermal Reservoiren_US
dc.subjectFluidsen_US
dc.subjectStable İsotopesen_US
dc.subjectWestern Anatoliaen_US
dc.subjectKizildereen_US
dc.subjectWestern Anatoliaen_US
dc.subjectSystemsen_US
dc.titleCharacterization and Comparison of geothermal fluids geochemistry within the Kizildere Geothermal Field in Turkey: New findings with power capacity expanding studiesen_US
dc.typeArticleen_US

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