using a simple coupled model for sediment transport and downstream partitioning of grain sizes. In the most traditional school, an increase size, and s is the sediment specific gravity C. Paola, P. L. Heller and C. L. Angevine i.
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Preview Paola et al. Basin Research, 1992
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using a simple coupled model for sediment transport and downstream partitioning of grain sizes. In the most traditional school, an increase size, and s is the sediment specific gravity C. Paola, P. L. Heller and C. L. Angevine i.
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