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1. The document discusses the inception of suspended sediment motion in rivers. It provides criteria for determining whether sediment motion will occur as bedload, saltation, or full suspension. 2. The critical bed shear stress must be exceeded for sediment motion to begin. Suspended sediment load occurs when the shear velocity divided by the particle fall velocity is approximately 1 based on empirical relationships. 3. Hyperconcentrated flows with sediment concentrations over 1% by volume are also discu

Author

salt2009

Language

EN