Hydrogeochemical and Isotopic Study of Groundwater in a Semi-arid Region: Yeniceoba Plain (Cihanbeyli-KONYA), Central Anatolia,Turkey

Basit Öğe Kaydı
dc.contributor.authorBozdag, Ayla
dc.contributor.authorGocmez, Giiler
dc.date.accessioned2020-03-26T19:24:33Z
dc.date.available2020-03-26T19:24:33Z
dc.date.issued2016
dc.departmentSelçuk Üniversitesien_US
dc.description.abstractGroundwater is the most important source of water supply in the Yeniceoba Plain in Central Anatolia, Turkey. An understanding of the geochemical evolution of groundwater is important for the sustainable development of water resources in this region. A hydrogeochemical investigation was conducted in the Plio-Quaternary aquifer system using stable isotopes (delta O-18 and delta D), tritium (H-3), major and minor elements (Ca, Na, K, Mg, Cl, SO4, NO3, HCO3 and Br) in order to identify groundwater chemistry patterns and the processes affecting groundwater mineralization in this system. The chemical data reveal that the chemical composition of groundwater in this aquifer system is mainly controlled by rock/water interactions including dissolution of evaporitic minerals, weathering of silicates, precipitation/dissolution of carbonates, ion exchange, and evaporation. Based on the values of Cl/Br ratio (> 300 mg/l) in the Plio-Quaternary groundwater, dissolution of evaporitic minerals in aquifer contributes significantly to the high mineralization. The stable isotope analyses indicate that the groundwater in the system was influenced by evaporation of rainfall during infiltration. Low tritium values (generally <1 tritium units) of groundwater reflect a minor contribution of recent recharge and groundwater residence times of more than three or four decades.en_US
dc.description.sponsorshipSelcuk University Scientific Research Projects (BAP)(Konya, Turkey)Selcuk University [07101034]en_US
dc.description.sponsorshipThis study was financially supported by Selcuk University Scientific Research Projects (BAP) (Project no. 07101034) (Konya, Turkey).en_US
dc.identifier.doi10.1111/1755-6724.12654en_US
dc.identifier.endpage241en_US
dc.identifier.issn1000-9515en_US
dc.identifier.issn1755-6724en_US
dc.identifier.issue1en_US
dc.identifier.scopusqualityQ3en_US
dc.identifier.startpage230en_US
dc.identifier.urihttps://dx.doi.org/10.1111/1755-6724.12654
dc.identifier.urihttps://hdl.handle.net/20.500.12395/33677
dc.identifier.volume90en_US
dc.identifier.wosWOS:000371440500018en_US
dc.identifier.wosqualityQ3en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherWILEYen_US
dc.relation.ispartofACTA GEOLOGICA SINICA-ENGLISH EDITIONen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.selcuk20240510_oaigen_US
dc.subjecthydrochemistryen_US
dc.subjectstable isotopesen_US
dc.subjecttritiumen_US
dc.subjectYeniceoba Plainen_US
dc.subjectCentral Anatoliaen_US
dc.titleHydrogeochemical and Isotopic Study of Groundwater in a Semi-arid Region: Yeniceoba Plain (Cihanbeyli-KONYA), Central Anatolia,Turkeyen_US
dc.typeArticleen_US

Dosyalar

Koleksiyon

WoS İndeksli Yayınlar Koleksiyonu
Scopus İndeksli Yayınlar Koleksiyonu