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.authorAfsin, M
dc.date.accessioned2019-08-01T13:38:39Z
dc.date.available2019-08-01T13:38:39Z
dc.date.issued2000
dc.departmentNiğde ÖHÜ
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 (O-18, H-2, H-3) studies. The springs have high discharge (Q>100 1/s) and low ion concentrations because of fast circulation along the groundwater flow path in the aquifer. Furthermore, because it has hydrochemical facies, it conforms Ca-Na-Mg-HCO3 hydrochemical facies, it conforms to high standards of drinking and irrigation water.
dc.identifier.endpage1196
dc.identifier.issn0943-0105
dc.identifier.issue10
dc.identifier.scopus2-s2.0-0034282028
dc.identifier.scopusqualityN/A
dc.identifier.startpage1190
dc.identifier.urihttps://hdl.handle.net/11480/5771
dc.identifier.volume39
dc.identifier.wosWOS:000089617800014
dc.identifier.wosqualityQ3
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.institutionauthorAfsin, M
dc.language.isoen
dc.publisherSPRINGER
dc.relation.ispartofENVIRONMENTAL GEOLOGY
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/closedAccess
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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