FEASIBILITY STUDY OF THE KOCABASLAR GEOTHERMAL FIELD (LAPSEKI/CANAKKALE/TURKEY)

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dc.contributor.authorDeniz, Ozan
dc.contributor.authorBozcu, Mustafa
dc.contributor.authorAtes, Ozkan
dc.date.accessioned2025-01-27T21:05:54Z
dc.date.available2025-01-27T21:05:54Z
dc.date.issued2016
dc.departmentÇanakkale Onsekiz Mart Üniversitesi
dc.description16th International Multidisciplinary Scientific Geoconference (SGEM 2016) -- JUN 30-JUL 06, 2016 -- Albena, BULGARIA
dc.description.abstractThe aim of this study is to research geothermal potential of the Kocabaslar hot spring. Geological, hydrogeological and geophysical investigations were conducted related to topic around the hot spring. Lithological units which composed of Eocene volcanics, Eocene sedimentary rocks and Quaternary alluvium were determined in the geological study. There are many tectonic lines in the region. Kocabaslar hot spring flows up through approximately E-W trending normal fault zone. Hydrogeological field measurements show that discharge, temperature, electrical conductivity, Eh and ph values of this hot spring are 0.5 L/s, 36 degrees C, 1212 microS/cm, 67 mV and 7.8, respectively, Electrical conductivity, discharge and temperature values are low. According to the chemical analysis results of samples taken from the hot and cold groundwater in the field, geothermal water is Na-Ca-SO4-HCO3 type and cold water generally Ca-Mg-HCO3-CO3 type. Thermal water is mixing with highly cold groundwater along the flow path. Results of isotope analysis (Oxygene-18, Deuterium and Tritium) show that this thermal water is at least older than 40 years and meteoric origin. Geophysical measurements (resistivity and induced polarization (IP) methods) were carried out along the 5 lines. Resistivity and chargeability cross sections were prepared using the inverse solution techniques. These cross sections and other data indicate that geothermal fluid may occur in the particular points and depths. There is any geothermal well drilled in this site before. Because of this reason there is a little knowledge about the geothermal potential of the geological units. It is suitable narrow drilling at least one point to research and develop of this geothermal field.
dc.description.sponsorshipBulgarian Acad Sci,Acad Sci Czech Republ,Latvian Acad Sci,Polish Acad Sci,Russian Acad Sci,Serbian Acad Sci & Arts,Slovak Acad Sci,Natl Acad Sci Ukraine,Inst Water Problem & Hydropower NAS KR,Natl Acad Sci Armenia,Sci Council Japan,World Acad Sci,European Acad Sci Arts & Lett,Acad Sci Moldova,Montenegrin Acad Sci & Arts,Croatian Acad Sci & Arts,Georgian Natl Acad Sci,Acad Fine Arts & Design Bratislava,Turkish Acad Sci,Bulgarian Ind Assoc,Bulgarian Minist Environm & Water
dc.identifier.endpage387
dc.identifier.isbn978-619-7105-63-6
dc.identifier.issn1314-2704
dc.identifier.startpage383
dc.identifier.urihttps://hdl.handle.net/20.500.12428/27833
dc.identifier.wosWOS:000391348600049
dc.identifier.wosqualityN/A
dc.indekslendigikaynakWeb of Science
dc.language.isoen
dc.publisherStef92 Technology Ltd
dc.relation.ispartofEnergy and Clean Technologies Conference Proceedings, Sgem 2016, Vol I
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.snmzKA_WoS_20250125
dc.subjectGeothermal
dc.subjectHydrogeochemistry
dc.subjectIsotope
dc.subjectKocabaslar
dc.subjectCanakkale
dc.titleFEASIBILITY STUDY OF THE KOCABASLAR GEOTHERMAL FIELD (LAPSEKI/CANAKKALE/TURKEY)
dc.typeConference Object

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