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Hydrochemical evolution and water quality along the groundwater flow path in the Sandikli plain, Afyon, Turkey

Access

info:eu-repo/semantics/closedAccess

Date

1997

Author

Afsin, M

Metadata

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Abstract

An 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.

Source

ENVIRONMENTAL GEOLOGY

Volume

31

Issue

3.Nis

URI

https://hdl.handle.net/11480/5834

Collections

  • Makale Koleksiyonu [2055]
  • Öksüz Yayınlar Koleksiyonu - WoS [2361]



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Ömer Halisdemir Üniversitesi Sabiha Şahenk Kütüphane ve Dokümantasyon Daire Başkanlığı, Niğde, Turkey
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