Hydrogeochemical characteristics of groundwater of the upper Carboniferous-lower permian aquifer system of the dnipro-donets depression South-Eastern part
DOI:
https://doi.org/10.15587/2313-8416.2014.30737Keywords:
salt dome structures, groundwater, brine, terrigenious formation, rock salt formationAbstract
Ground water within the researched area is characterized by considerable variability of salinity, macro-and microcomponents content. . To determine the mechanisms of formation of hydrochemical "anomalies" has been created the isoline maps of salinity, Na/Cl coefficient and other hydrological characteristics of groundwater. Based on analysis of lithological and paleohydrological data maps the conditions of groundwater chemical composition in area and in the context has been determined as different.
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