## Abstract Sediment transport in rill flows exhibits the characteristics of nonβequilibrium 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
Sediment Transport Model for Seepage Erosion of Streambank Sediment
β Scribed by Fox, G. A.; Wilson, G. V.; Periketi, R. K.; Cullum, R. F.
- Book ID
- 120823903
- Publisher
- American Society of Civil Engineers
- Year
- 2006
- Tongue
- English
- Weight
- 469 KB
- Volume
- 11
- Category
- Article
- ISSN
- 1084-0699
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