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A Role of Sediment Transport in Alluvial Channels
Once a critical amount of sediment is being moved in an alluvial channel, velocity can be expressed as a function of slope and of size and composition of the moving sediment load. Depth is a redundant parameter. At sediment transport rates below critical, depth is an effective parameter. Methods of determining the size and composition of the moving sediment load are analyzed as is the problem of determining when depth becomes redundant. The phenomena of fill and scour at alluvial channel sections is also considered.
A Role of Sediment Transport in Alluvial Channels
Once a critical amount of sediment is being moved in an alluvial channel, velocity can be expressed as a function of slope and of size and composition of the moving sediment load. Depth is a redundant parameter. At sediment transport rates below critical, depth is an effective parameter. Methods of determining the size and composition of the moving sediment load are analyzed as is the problem of determining when depth becomes redundant. The phenomena of fill and scour at alluvial channel sections is also considered.
A Role of Sediment Transport in Alluvial Channels
Maddock, Thomas (author)
Journal of the Hydraulics Division ; 99 ; 1915-1931
2021-01-01
171973-01-01 pages
Article (Journal)
Electronic Resource
Unknown
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