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This paper outlines the various approaches used to calculate bedload transport. As bedload transport exhibits considerable spatial and temporalvariations, computing the bedload transport rates and morphological changes experienced by streambeds is difficult. A large body of experi-mental work has revealed scaling laws relating the mean transport rate qs to hydraulic conditions.
Mehrdad Kiani Oshtorjani, Zhipeng Li, Yong Zhang
Giovanni De Cesare, Severin Stähly, Christian Mörtl, Robin Schroff