Hydrochemical evolution and water quality along the groundwater flow path in the Sandikli plain, Afyon, 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.issued1997
dc.departmentNiğde ÖHÜ
dc.description.abstractAn unconfined aquifer system suggests an open system in the study area. Hydrochemical evolution is related to the flow path of groundwater. The groundwaters are divided into two hydrochemical facies in the study area, 1) Ca-Mg-HCO3 and 2) Ca-Mg-SO4HCO3. Facies 1 has shallow (young) waters which dominate in recharge areas during rapid flow conditions, whereas facies 2 may show shallow and mixed waters which dominate intermediate or discharge areas during low 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.endpage230
dc.identifier.issn0177-5146
dc.identifier.issue45385
dc.identifier.scopus2-s2.0-0030619223
dc.identifier.scopusqualityN/A
dc.identifier.startpage221
dc.identifier.urihttps://hdl.handle.net/11480/5834
dc.identifier.volume31
dc.identifier.wosWOS:A1997XF98000012
dc.identifier.wosqualityQ3
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.institutionauthorAfsin, M
dc.language.isoen
dc.publisherSPRINGER VERLAG
dc.relation.ispartofENVIRONMENTAL GEOLOGY
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subjecthydrochemical evolution
dc.subjectunconfined aquifer
dc.subjectfacies
dc.subjectshallow water
dc.subjectresidence time
dc.titleHydrochemical evolution and water quality along the groundwater flow path in the Sandikli plain, Afyon, Turkey
dc.typeArticle

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