Hydrochemical evolution and water quality along the groundwater flow path in the Sandikli plain, Afyon, Turkey
Küçük Resim Yok
Tarih
1997
Yazarlar
Dergi Başlığı
Dergi ISSN
Cilt Başlığı
Yayıncı
SPRINGER VERLAG
Erişim Hakkı
info:eu-repo/semantics/closedAccess
Özet
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.
Açıklama
Anahtar Kelimeler
hydrochemical evolution, unconfined aquifer, facies, shallow water, residence time
Kaynak
ENVIRONMENTAL GEOLOGY
WoS Q Değeri
Q3
Scopus Q Değeri
N/A
Cilt
31
Sayı
45385
