Determination of the origin of the Helvadere drinking springs by means of hydrochemical and isotopic techniques, Aksaray, Central Anatolia, Turkey
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Tarih
2000
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Yayıncı
Springer-Verlag GmbH & Company KG, Berlin
Erişim Hakkı
info:eu-repo/semantics/openAccess
Özet
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.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.
Açıklama
Anahtar Kelimeler
Drinking Spring, Fast Circulation, Helvadere, Hydrochemical Facies, Isotope, Volcanic Aquifer
Kaynak
Environmental Geology
WoS Q Değeri
Scopus Q Değeri
N/A
Cilt
39
Sayı
10
