Transient transport phenomena can be determined in a given river reach by “constrained” sediment boundary conditions which can arise either from the presence of a man-made structural intervention or from the variation of inflow sediment rate upstream of an alluvial channel reach.
Termini, D. (2014). Nonuniform sediment transport and flow characteristics downstream of a hydraulic structure. In Hydrology in a Changing World: Environmental and Human Dimensions.
Nonuniform sediment transport and flow characteristics downstream of a hydraulic structure
TERMINI, Donatella
2014-01-01
Abstract
Transient transport phenomena can be determined in a given river reach by “constrained” sediment boundary conditions which can arise either from the presence of a man-made structural intervention or from the variation of inflow sediment rate upstream of an alluvial channel reach.
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