Gravel threshold of motion: a state function of sediment transport disequilibrium?
In most sediment transport models, a threshold variable dictates the shear stress at which non-negligible bedload transport begins. Previous work has demonstrated that nondimensional transport thresholds (<i>τ</i><sub>c</sub>*) vary with many factors related not only to grain...
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2016-08-01
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| Series: | Earth Surface Dynamics |
| Online Access: | http://www.earth-surf-dynam.net/4/685/2016/esurf-4-685-2016.pdf |