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Transport capacity models for unsteady and non-equilibrium sediment transport in alluvial channels

✍ Scribed by Gokmen Tayfur; Vijay P. Singh

Book ID
116376308
Publisher
Elsevier Science
Year
2012
Tongue
English
Weight
848 KB
Volume
86
Category
Article
ISSN
0168-1699

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## Abstract Sediment transport in rill flows exhibits the characteristics of non‐equilibrium transport, and the sediment transport rate of rill flow gradually recovers along the flow direction by erosion. By employing the concept of partial equilibrium sediment transport from open channel hydraulic