supported by grants from the National Key Research and Development Program of China (2017YFC0405504);the National Natural Science Foundation of China (51179211);the Basic Research Special Fund of IWHR (SE0145B142017)
Although thin on the order of several to tens of millimeters, sheet flows normally comprise a lower pick- up sub-layer and an upper contact-load sub-layer, separated at the bed level (z = 0). The time-averaged conce...
supported by the National Natural Science Foundation of China(Grant No.51179211)
Wave shapes that induce velocity skewness and acceleration asymmetry are usually responsible for onshore sediment transport, whereas undertow and bottom slope effect normally contribute to offshore sediment transport....