Abstract

Spatial variations of the chemical composition of the Volga River delta waters and its interannual variability were estimated on the basis of long-term data on the content of macro components, biogenic ele-ments, and trace elements. It was shown that the significant transformation inside the delta is peculiar only to the biogenic element runoff, which is influenced by production–destruction processes, whereas the migra-tion of the major ions and dissolved trace elements in the delta watersheds occurs without any essential vari-ations.

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