Hydrogeochemistry and groundwater quality evaluation along the groundwater flow path in unconfined aquifer in Hankendi Plain, Elazig, Turkey

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dc.contributor.authorÇetindag, B
dc.contributor.authorÜnsal, N
dc.date.accessioned2026-08-12T17:13:15Z
dc.date.issued2004
dc.departmentFırat Üniversitesi
dc.description.abstractThe study area is located to the west of Elazig, in southeastern Turkey. Hydrochemical evolution of the groundwater is related to the flow path of groundwater. The groundwater in the unconfined aquifer may be classified in terms of Ca-Mg-HCO3 hydrochemical facies characterised by shallow (young) waters which dominate the recharge areas during rapid flow conditions. Ionic concentrations, TDS, EC and water quality are related to groundwater residence time and groundwater types. The groundwaters in the plain are chemically potable and suitable for both domestic and agricultural purposes.
dc.identifier.endpage203
dc.identifier.issn0016-7622
dc.identifier.issn0974-6889
dc.identifier.issue2
dc.identifier.scopus2-s2.0-2942683003
dc.identifier.scopusqualityQ2
dc.identifier.startpage191
dc.identifier.urihttps://hdl.handle.net/11508/51350
dc.identifier.volume63
dc.identifier.wosWOS:000188795400006
dc.identifier.wosqualityQ3
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherGeological Soc India
dc.relation.ispartofJournal of the Geological Society of India
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.snmzKA_WoS_20260511
dc.subjecthydrogeochemistry
dc.subjectunconfined aquifer
dc.subjectwater quality
dc.subjectElazig
dc.subjectTurkey
dc.titleHydrogeochemistry and groundwater quality evaluation along the groundwater flow path in unconfined aquifer in Hankendi Plain, Elazig, Turkey
dc.typeArticle

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