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- W63722123 abstract "A conceptual model of downstream change in river bank erosion is presented that indicates scale to be an important control of the many dominant retreat processes. The model predicts that in upstream reaches, where banks are small and stream power is low, sub-aerial preparation processes are most effective. In mid-basin areas, combining individual functions for spatial change in discharge and slope suggests that stream power peaks and fluid entrainment mechanisms prevail. In the lowest reaches, where materials are cohesive and resistant to fluid shear, bank heights exceed critical geotechnical instability thresholds and the most important bank process is mass failure. Experiments and literature suggest that the modeling approach helps rationalize the variety of process conclusions reached by other workers, which has implications for understanding the nature, rate and timing of sediment transfer from channel sides to rivers." @default.
- W63722123 created "2016-06-24" @default.
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- W63722123 date "2008-01-01" @default.
- W63722123 modified "2023-09-26" @default.
- W63722123 title "The impact of scale on the processes of channel-side sediment supply: a conceptual model" @default.
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