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- W4310349758 abstract "Alluvial channels are continuously modified by sediment movement and exist in comparative equilibrium. The longitudinal profiles and cross-sections of these channels depend on hydraulic and sediment factors and boundary conditions which govern channel morphology. This chapter discusses the theory of channel mobility leading to stable hydraulic geometry." @default.
- W4310349758 created "2022-12-09" @default.
- W4310349758 date "2022-12-08" @default.
- W4310349758 modified "2023-09-27" @default.
- W4310349758 title "Channel Mobility Theory" @default.
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- W4310349758 doi "https://doi.org/10.1017/9781009222136.013" @default.
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