Abstract
Itakura and Kishi's theory about open channel flows with suspended sediment predicts decreasing of the friction factors for rough beds. While, for smooth beds, Imamoto et. al. observed increasing of them. However, from the fact that the important property of the flow, the increase of velocity gradient observed also for the smooth bed, decreasing of the integrated constant A of log low velocity profile was deduced. In this paper we proposed a model to explain the phenomena due to a modification of the coherent structure near the all by the suspended sediment
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