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- W1990255909 abstract "The analysis of a laboratory and field data set for sand-bed channels defines the characteristics of upper-regime plane bed with sediment transport. The occurrence of upper-regime plane bed relates to the laminar sublayer thickness δ and depends on shear velocity u*, median grain size d50, and grain shear Reynolds number R*. Two different boundary conditions are recognized: (1) Transition to hydraulically smooth when R* < 11.6; and (2) transition to hydraulically rough when R* > 11.6. In the first case, upper-regime plane bed is obtained when u*2≅gδ, where g is the gravitational acceleration. In the second case, upper-regime plane bed is observed when d50≅ 2δ. Temperature effects are possible when R* approaches 11.6, which explains the observations on the Missouri River. Resistance to flow for plane bed with sediment transport increases with the Shields parameter." @default.
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- W1990255909 date "1998-11-01" @default.
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- W1990255909 title "Upper-Regime Plane Bed" @default.
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- W1990255909 doi "https://doi.org/10.1061/(asce)0733-9429(1998)124:11(1086)" @default.
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