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- W23376765 abstract "Sediment acts in two contrasting ways in the erosion of bedrock rivers. Firstly, there is a ‘tools’ effect whereby grains in transport impact and abrade the bed, and, secondly, a ‘cover’ effect in which deposited sediment protects the bed from erosion. The bed erosion rate depends on the balance between these two effects, which is known to be a function of factors including sediment supply and shear stress. Possible forms of this relationship have been presented by Sklar and Dietrich (2004, 2006) and Turowski et al. (2007); further testing and validation of the suggested relationships are however necessary. Grain interactions are known to exert an important control over sediment transport in alluvial rivers and a limitation of current bedrock erosion relationships is that whilst they consider the grain-scale dynamics of grain saltation, they do not consider the grain-scale interactions that influence sediment entrainment." @default.
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- W23376765 date "2009-04-01" @default.
- W23376765 modified "2023-09-24" @default.
- W23376765 title "The action of sediment in bedrock river erosion" @default.
- W23376765 hasPublicationYear "2009" @default.
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