Hydrological Properties of the Derme Karstic Springs by Using Hydrogeochemical Analyses and Environmental Isotope Techniques

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dc.authoridDursun, Omer Faruk/0000-0003-3923-5205
dc.authoridFIRAT, Mahmut/0000-0002-8010-9289
dc.authorwosidDursun, Omer Faruk/AAA-8464-2020
dc.authorwosidÇeliker, Murat/JZT-7970-2024
dc.contributor.authorDursun, Omer Faruk
dc.contributor.authorCeliker, Murat
dc.contributor.authorFirat, Mahmut
dc.date.accessioned2024-08-04T20:41:28Z
dc.date.available2024-08-04T20:41:28Z
dc.date.issued2016
dc.departmentİnönü Üniversitesien_US
dc.description.abstractIn this study, determination of recharging mechanism of the Derme karst spring by hydrogeochemical analysis and environmental isotope techniques are aimed. The Derme karst spring is an important karst spring that is located in the eastern part of Turkey, meets the domestic water need of Malatya province having a population of 750000, and has an average flow rate of 2.7m(3)/s. Water samples were taken from eight different springs from May to October 2011 for physicochemical and isotopic analyses (oxygen 18, deuterium, tritium) in order to determine the catchment mechanisms and the hydrodynamic structures of these karstic springs. The hydrogeochemical classification of spring waters was performed through a piper diagram. The results indicated that all of the springs were characterized by the calcium bicarbonate type. It was found that the deuterium excess value of the karstic springs was ranging from 13.42 to 18.84%, and that these springs were fed by both territorial and marine origin rainfalls. It was considered that the springs in the karstic region were under the influence of different karstic systems.en_US
dc.description.sponsorshipIUBAP (Inonu University Scientific Projects Unit) [2011/46]en_US
dc.description.sponsorshipThis research was supported by IUBAP (Inonu University Scientific Projects Unit) under the project number of 2011/46. The authors are grateful to the Editor and Anonymous Reviewers for their helpful and constructive comments on an earlier draft of this paper.en_US
dc.identifier.doi10.1002/clen.201400035
dc.identifier.issn1863-0650
dc.identifier.issn1863-0669
dc.identifier.issue2en_US
dc.identifier.scopus2-s2.0-84956762449en_US
dc.identifier.scopusqualityQ3en_US
dc.identifier.urihttps://doi.org/10.1002/clen.201400035
dc.identifier.urihttps://hdl.handle.net/11616/97149
dc.identifier.volume44en_US
dc.identifier.wosWOS:000369959600004en_US
dc.identifier.wosqualityQ3en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherWiley-Blackwellen_US
dc.relation.ispartofClean-Soil Air Wateren_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectGeographic information system (GIS)en_US
dc.subjectHydrogeologyen_US
dc.subjectIsotopesen_US
dc.subjectKarstic groundwateren_US
dc.subjectWater managementen_US
dc.titleHydrological Properties of the Derme Karstic Springs by Using Hydrogeochemical Analyses and Environmental Isotope Techniquesen_US
dc.typeArticleen_US

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