Abstract
The presented results constitute a summary of a five-year study conducted from 2009 to 2013 in the upper catchment of the Lewinska Struga stream. Weekly research on the physical and chemical properties of Lewinska Struga waters at the Domyslow profile was combined with seasonal hydrochemical studies conducted in the following five flow-through lakes : Warnowo, Rabiąz, Czajcze, Domyslowskie and Żolwinskie. Across young glacial areas of the Polish Lowland, a drainage network is often produced by a fluvial-lacustrine system, in which a river links subsequent lakes via short sections. In such cases, this fluvial transport of solutes is sometimes disturbed in lakes, which are both their source and deposition area. The main research strategy of the paper was aimed at determining the functioning of the fluvial-lacustrine system of Lewinska Struga stream on Wolin Island. This paper also discusses the dynamics of fluvial transport of solutes carried with Lewinska Struga waters.
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