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In floodplain ponds with brief potamophases focused at the beginning of a hydrologic year, liquid quality typical for interzonal ponds had been seen; in floodplain lakes utilizing the longest potamophases with their concentration at the end of a hydrologic year, ionic concentrations typical of extrazonal lakes happened, whereas in lakes with a potamophase period close to the normal price and a spring concentration of floods, advanced liquid quality was observed, typical of mixoz