Abstract
The article presents data on the influence of waters from the self-flowing wells in the floodplain of the Aremzyanka river of the first order inflow on the chemical composition of the water in the large transboundary Irtysh river in the south of the Tyumen region (Tobolsk District). The article shows the excess of the background of various elements in the bottom sediments of the studied rivers. The number of ions in the water of the Aramzyanka river is 2 times higher in comparison with the main river. The paper discusses the impact of saline water from a flowing well on a freshwater ecosystem, its components.
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