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Field studies of sediment transport by overland flow

โœ Scribed by R. P. C. Morgan

Publisher
John Wiley and Sons
Year
1980
Tongue
English
Weight
623 KB
Volume
5
Category
Article
ISSN
0360-1269

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๐Ÿ“œ SIMILAR VOLUMES

Evaluating overland flow sediment transp
Evaluating overland flow sediment transport capacity
โœ Vito Ferro ๐Ÿ“‚ Article ๐Ÿ“… 1998 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 276 KB

An equation for evaluating the sediment transport capacity of overland ยฏow is a necessary part of a physically based soil erosion model describing sediment detachment and transport as distributed processes. At ยฎrst, for the hydraulic conditions of small-scale and large-scale roughness, the sediment

Predicting sediment transport by interri
Predicting sediment transport by interrill overland flow on rough surfaces
โœ Abrahams, Athol D.; Li, Gary; Krishnan, Chitra; Atkinson, Joseph F. ๐Ÿ“‚ Article ๐Ÿ“… 1998 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 196 KB ๐Ÿ‘ 1 views

Modelling soil erosion requires an equation for predicting the sediment transport capacity by interrill overland flow on rough surfaces. The conventional practice of partitioning total shear stress into grain and form shear stress and predicting transport capacity using grain shear stress lacks rigo

Sediment transport by overland flow over
Sediment transport by overland flow over an area of net deposition
โœ L. Beuselinck; G. Govers; A. Steegen; T. A. Quine ๐Ÿ“‚ Article ๐Ÿ“… 1999 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 217 KB ๐Ÿ‘ 1 views

Flume studies were conducted in order to evaluate the inยฏuence of slope, sediment size, discharge and inยฏow sediment concentration on sediment deposition by overland ยฏow. Additionally, experiments were carried out to measure transport capacity of overland ยฏow at low slopes, using a wide range of dis

Sediment-transport competence of rain-im
Sediment-transport competence of rain-impacted interrill overland flow
โœ Parsons, Anthony J.; Stromberg, Simon G. L.; Greener, Mark ๐Ÿ“‚ Article ๐Ÿ“… 1998 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 459 KB ๐Ÿ‘ 1 views

Laboratory experiments to determine the maximum size of sediment transported in shallow, rain-impacted flow were conducted in a recirculating flume 4โ€ข80 m long and 0โ€ข50 m wide. Rainfall intensities were varied between 51 and 138 mm h -1 , flow was introduced from a header tank into the flume at rate