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• W2080406952 startingPage "46" @default.
• W2080406952 abstract "Hydrochemical, multivariate statistical and inverse hydrogeochemical modeling techniques were used to determine the main factors and mechanisms controlling the chemistry of groundwaters in the El Eulma Mio-Plio-Quaternary aquifer, East Algeria. Cluster analysis based on major ion contents defined three main chemical water types, reflecting different hydrochemical processes. The first, group 1, has low salinity (mean EC = 937 μS/cm) and abundance orders Ca2+ > Na+ ≈ Mg2+ > K+ and HCO3+>Cl->SO42->NO3-. With increased water–rock interaction, waters in groups 2 and 3 become more saline, changing composition towards Cl–HCO3–Ca and Cl–Ca–Na types. The PHREEQC geochemical modeling demonstrated that relatively few phases are required to derive water chemistry in the area. In a broad sense, the reactions responsible for the hydrochemical evolution in the area fall into three categories: (1) dissolution of evaporite minerals; (2) precipitation of carbonate minerals, quartz, kaolinite and Ca-smectite; (3) ion exchange." @default.
• W2080406952 created "2016-06-24" @default.
• W2080406952 creator A5026666217 @default.
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• W2080406952 date "2012-05-01" @default.
• W2080406952 modified "2023-10-01" @default.
• W2080406952 title "Geochemical evolution of groundwater in an alluvial aquifer: Case of El Eulma aquifer, East Algeria" @default.
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• W2080406952 doi "https://doi.org/10.1016/j.jafrearsci.2012.03.001" @default.
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