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In this paper, a simulation method is developed to predict sedimentation process in a reservoir. This model can calculate the temporal variation of bed elevation, sediment discharge, and vertical grain size distribution in deposits. Water and sediment discharge as the boundary conditions at the upstream end, are obtained from a sediment runoff model. In this model, the watershed is constituted by several slope units and channel network. Sediment runoff is simulated by using governing equations which correspond to each flow regime such as a debris flow, an immature debris flow, and a turbulent flow. These models are applied to the actual mountainous watershed, the Fudosawa and Nigorisawa River, Nagano Prefecture.

PREDICTION OF SEDIMENTATION PROCESS IN A RESERVOIR USING A SEDIMENT RUNOFF MODEL