Numerical Simulation of the Propagation of Fine-Grained Sediment Pulses in Alluvial Rivers
Sediment pulses are defined as large amounts of loose sediment that are suddenly deposited in river corridors due to the action of external factors or processes of natural or anthropogenic origin. Such factors and processes include landslides, debris flows from tributaries, volcanic eruptions, dam r...
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| Format: | Others |
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Virginia Tech
2018
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| Online Access: | http://hdl.handle.net/10919/82348 |