Please use this identifier to cite or link to this item: https://hdl.handle.net/11147/2572
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dc.contributor.authorBaba, Alper-
dc.contributor.authorYüce, Galip-
dc.contributor.authorDeniz, Ozan-
dc.contributor.authorYasin, Didem-
dc.date.accessioned2016-12-05T12:59:03Z
dc.date.available2016-12-05T12:59:03Z
dc.date.issued2009-06
dc.identifier.citationBaba, A., Yüce, G., Deniz, O., and Yasin, D. (2009). Hydrochemical and isotopic composition of Tuzla geothermal field (Canakkale-Turkey) and its environmental impacts. Environmental Forensics, 10(2), 144-161. doi:10.1080/15275920902873418en_US
dc.identifier.issn1527-5922
dc.identifier.issn1527-5922-
dc.identifier.urihttp://dx.doi.org/10.1080/15275920902873418
dc.identifier.urihttp://hdl.handle.net/11147/2572
dc.description.abstractTuzla is an active geothermal area located in northwestern Turkey, 80 km south of the city of Canakkale and 5 km from the Aegean Coast. Geothermal brine, deriving from this area, contains an abundance of NaCl and a water temperature of 173°C (T1 well at 814 m depth) is typically encountered. The aim of this study was to determine the hydrogeochemical properties of the geothermal brine using both chemical and isotopic data, and to investigate the origin of the geothermal brine in the Tuzla area and the environmental impacts of Tuzla Geothermal Field (TGF). Both geothermal brine and shallow groundwater in the area are of meteoric origin. Isotope results indicate that the hot saline waters (brine) in the Tuzla geothermal field originate from connate water along faults. As the saline water rises to the surface, it mixes with shallow groundwaters in various ratios. In addition, the high sodium (Na) and chloride (Cl) content in the Tuzla Stream, fed from the Tuzla geothermal brine during the dry season, cause an increase in sodium and chloride concentrations in the shallow groundwaters by infiltration into the aquifer. Moreover, salt accumulation on the surface is observed due to the uncontrolled artesian flow of geothermal brine, which adversely affects the salinity of shallow groundwater.en_US
dc.description.sponsorshipTÜBİTAKen_US
dc.language.isoenen_US
dc.publisherTaylor and Francis Ltd.en_US
dc.relation.ispartofEnvironmental Forensicsen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectDeuteriumen_US
dc.subjectGeothermal fluiden_US
dc.subjectHydrogeochemistryen_US
dc.subjectOxygen-18en_US
dc.subjectTritiumen_US
dc.subjectTuzlaen_US
dc.titleHydrochemical and isotopic composition of Tuzla geothermal field (Canakkale-Turkey) and its environmental impactsen_US
dc.typeArticleen_US
dc.authoridTR18248en_US
dc.institutionauthorBaba, Alper-
dc.departmentIzmir Institute of Technology. Civil Engineeringen_US
dc.identifier.volume10en_US
dc.identifier.issue2en_US
dc.identifier.startpage144en_US
dc.identifier.endpage161en_US
dc.identifier.wosWOS:000275923300006en_US
dc.identifier.scopus2-s2.0-70449411699en_US
dc.relation.tubitakinfo:eu-repo/grantAgreement/TUBITAK/CAYDAG/103Y010en_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.identifier.doi10.1080/15275920902873418-
dc.relation.doi10.1080/15275920902873418en_US
dc.coverage.doi10.1080/15275920902873418en_US
dc.identifier.scopusqualityQ2-
item.fulltextWith Fulltext-
item.openairetypeArticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.grantfulltextopen-
crisitem.author.dept03.03. Department of Civil Engineering-
Appears in Collections:Civil Engineering / İnşaat Mühendisliği
Scopus İndeksli Yayınlar Koleksiyonu / Scopus Indexed Publications Collection
Sürdürülebilir Yeşil Kampüs Koleksiyonu / Sustainable Green Campus Collection
WoS İndeksli Yayınlar Koleksiyonu / WoS Indexed Publications Collection
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