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Groundwater chemistry of Quaternary aquifers has been studied in main water-well fields of Eastern Slavonia, Croatia. These alluvial sediments were deposited in the shallow lakes and swamps during the Middle and Upper Pleistocene. The reductive conditions of sedimentation prevailed. The groundwater composition shows the spatial and the temporal variations of basic cations and anions and of the concentrations of groundwater constituents (iron, manganese, arsenic, ammonia).
groundwater chemistry ; Quaternary aquifer ; Sava river catchment
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