Modes of Bed-Load Movement on a Smooth Rigid Surface
Sediment grains transported as supply-limited bed load on a rigid surface move either discretely or collectively as bed forms, with significantly different effective grain speeds and active storage volumes. The adopted mode has implications for sediment sorting and heavy mineral placer formation, di...
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Published in | Journal of hydraulic engineering (New York, N.Y.) Vol. 137; no. 10; pp. 1283 - 1286 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Reston, VA
American Society of Civil Engineers
01.10.2011
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Subjects | |
Online Access | Get full text |
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Summary: | Sediment grains transported as supply-limited bed load on a rigid surface move either discretely or collectively as bed forms, with significantly different effective grain speeds and active storage volumes. The adopted mode has implications for sediment sorting and heavy mineral placer formation, dispersal of grain-associated pollutants, and accumulation and flushing of sediment deposits in unlined canals and sewers. The threshold condition between the two modes has been established for a smooth surface from flume experiments with different sediment types, flow conditions, and sediment supply rates. This is expressed in terms of a relationship between the sediment movability number, a dimensionless bed load parameter, and a grain shear Reynolds number. |
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ISSN: | 0733-9429 1943-7900 |
DOI: | 10.1061/(ASCE)HY.1943-7900.0000400 |