Determination of the origin of the Helvadere drinking springs by means of hydrochemical and isotopic techniques, Aksaray, Central Anatolia, Turkey

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dc.contributor.authorAfşin, Mustafa
dc.date.accessioned13.07.201910:50:10
dc.date.accessioned2019-07-16T08:25:00Z
dc.date.available13.07.201910:50:10
dc.date.available2019-07-16T08:25:00Z
dc.date.issued2000
dc.departmentMühendislik Fakültesi
dc.description.abstractThe main aquifer of the Helvadere springs that emerges on the strike-slip of the Hasandagi fault set alongside the Tuzgolu (salt lake) fault zone, and trends in a NW-SE direction of Aksaray city, in the western part of Central Anatolia, is the exposed rocks of Hasandagi which are volcanics that have distinct hydrogeological properties. The meteoric origin of the spring waters is deduced from hydrochemical and environmental isotope ( 18 O, 2 H, 3 H) studies. The springs have high discharge (Q>100 l/s) and low ion concentrations because of fast circulation along the groundwater flow path in the aquifer. Furthermore, because it has Ca-Na-Mg-HCO 3 hydrochemical facies, it conforms to high standards of drinking and irrigation water.The main aquifer of the Helvadere springs that emerges on the strike-slip of the Hasandagi fault set alongside the Tuzgolu (salt lake) fault zone, and trends in a NW-SE direction of Aksaray city, in the western part of Central Anatolia, is the exposed rocks of Hasandagi which are volcanics that have distinct hydrogeological properties. The meteoric origin of the spring waters is deduced from hydrochemical and environmental isotope ( 18 O, 2 H, 3 H) studies. The springs have high discharge (Q>100 l/s) and low ion concentrations because of fast circulation along the groundwater flow path in the aquifer. Furthermore, because it has Ca-Na-Mg-HCO 3 hydrochemical facies, it conforms to high standards of drinking and irrigation water.
dc.description.sponsorshipAcknowledgements The author is grateful to the Scientific and Technical Research Council of Turkey (TÜBİTAK) for supporting the present research project, 195Y009 (YDABÇAG-120).
dc.identifier.doi10.1007/s002549900103
dc.identifier.endpage1196en_US
dc.identifier.issn0943-0105
dc.identifier.issue10en_US
dc.identifier.scopusqualityN/A
dc.identifier.startpage1190en_US
dc.identifier.urihttps://dx.doi.org/10.1007/s002549900103
dc.identifier.urihttps://hdl.handle.net/20.500.12451/2996
dc.identifier.volume39en_US
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherSpringer-Verlag GmbH & Company KG, Berlin
dc.relation.ispartofEnvironmental Geology
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/openAccess
dc.subjectDrinking Spring
dc.subjectFast Circulation
dc.subjectHelvadere
dc.subjectHydrochemical Facies
dc.subjectIsotope
dc.subjectVolcanic Aquifer
dc.titleDetermination of the origin of the Helvadere drinking springs by means of hydrochemical and isotopic techniques, Aksaray, Central Anatolia, Turkey
dc.typeArticle

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