In the direction of the frontal dam of the reservoir mean concentrations of substances dissolved in water were reduced while those of oxygen, phosphorus, and ammonium ions increased, bringing about distinct differences between the three parts of the impoundment, conditioned by the seasonality of water inflow to the reservoir. In summer and autumn in the different parts of the reservoir a similar chemical composition of waters was observed, while in winter and during the spring rise it was distinctly differentiated.