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- W184033169 abstract "Groundwater chemistry is largely a function of mineral composition, the formation through which it flows due to rock–water interaction. Evaporation and concentration, dilution due to precipitation also can change the chemical composition of groundwater but rock–water interaction is the major process because solid phases (inorganic and organic matter) are the primary sources and sinks of dissolved constituents of groundwater. During groundwater movement along its path from recharge to discharge areas, a variety of chemical reactions with solid phases take place. These chemical reactions varies spatially and temporally, depending on the chemical nature of the initial water, geological formations, and residence time. The resulting concentrations of major ions of groundwater can be used to identify the intensity of rock–water interaction and chemical reactions. Generally different chemical processes occur during rock-water interaction, which include dissolution/precipitation, ion exchange processes, oxidation, and reduction. Rock types are broadly classified as igneous, metamorphic, and sedimentary. Minerals present in these rocks completely or partially dissolve in water according to the resistance of chemical weathering. Occurrence and intensity of these chemical reactions depend on the initial water's disequilibrium with rocks in contact. During rock–water interaction a variety of chemical processes occur such as weathering and dissolution, ion exchange processes, oxidation, and reduction." @default.
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- W184033169 date "2007-01-01" @default.
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- W184033169 title "Chapter 11 Rock–water interaction and its control on chemical composition of groundwater" @default.
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- W184033169 doi "https://doi.org/10.1016/s1474-8177(07)05011-5" @default.
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