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This study is the first attempt in the literature on the subject ofcomparing water balance components for floodplain lake basins, depending onthe type of a lake connection to the parent river. Research was carried outin the Bug River valley in 2007–2011 water years. Four types of connectionswere distinguished in the area under study. Simple water balance equationcould only be used with regard to the lakes connected to the main river viathe upstream crevasses. Detailed and individual water balance equations weredeveloped with reference to the other types of lakes. Water gains and lossesvaried significantly in the lakes under study. Values of horizontal waterbalance components (inflow and outflow) of the floodplain lake in WolaUhruska considerably prevailed over the vertical ones (precipitation andevaporation). Inflow of the Bug River waters was diverse during the timeperiod under study and amounted from 600 000 to 2 200 000 m3 yr−1.Volumes of precipitation and evaporation were ratherstable and amounted to approx. 30 000 m3 yr−1. The lowestdisparity between horizontal and vertical water balance components wasobserved in the inter-levee lake. Both upstream inflow of rivers water andoutflow from the lake (ranged from 0 in 2008 to 35 000 m3 yr−1 in2009) were usually an order of magnitude higher than precipitation andevaporation from the lake surface (700–800 m3 yr−1). Study showedthat the values and the proportion between aforementioned vertical andhorizontal water balance elements were determined by the type of a lakeconnection to the Bug River. Storage volume showed no relationship to thetype of connection, but resulted from individual features of the lakes(location within the valley, precipitation and evaporation volume,difference between water inflow and outflow)

Water balance of selected floodplain lake basins in the Middle Bug River valley