Modelling sediment transport in stream c
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K. D. Sharma; J. S. R. Murthy
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Article
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1994
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John Wiley and Sons
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English
โ 318 KB
## Abstract Ephemeral channels in arid regions convey larger amounts of sediment than perennial channels in humid regions. Sediment graphs at the outlet of channels have been derived by the standard sediment rating curve technique and by a lumped model based on the instantaneous unit sediment graph