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On the basis of eight recorded rainfall-runoff-suspended sediment events in a small, agricultural catchment of the Zagożdżonka river, a ratio of runoff lag time (Lag) and lag time of sediment flow (Lags) was analysed. The first Lag time of them is defined as the elapsed time between the occurrence of centroid of eflective rainfall and the storm runoff hydrographs. The last one is defined as the elapsed...
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