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This paper formulates a generalized bottom‐boundary condition for nonequilibrium transport of sediment in terms of two parameters: the deposition velocity and the equilibrium bottom concentration. Theoretical expressions for the two parameters are derived. Analytical solution to the sediment transport equation, using the generalized bottom‐boundary condition, is also given. Finally, a number of available formulations of the bottom condition are reviewed and shown to be special cases of this generalized one.
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Kwokming James Cheng (1984) studied this question.
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