Abstract
Predicting the entrainment and transport rates of sediment grains making up an erodible bed underlying an arbitrary flow field requires a mechanistic understanding of the coupling between the flow and the forces on sediment grains. To help develop such an understanding, a suite of flow and sediment-transport experiments are described; these may be loosely divided into two categories. First, measurements of near-bed flow structure and sediment motion in a variety of spatially or temporally accelerating flows are used to show the manner in which changes in flow structure can impact sediment entrainment and transport. Second, direct high-frequency measurements of lift and drag on sediment particles in various turbulent flows are used to make a more direct connection between nearbed flow structure and sediment dynamics. Taken together, these experiments show how even changes in turbulence structure due to spatial and/or temporal accelerations can have a significant effect on the sediment-transport field. Finally, a method is briefly outlined for predicting sediment motion under arbitrary flows using either measured nearbed velocity time series or flow information predicted from direct numerical simulations or large-eddy simulations.
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Nelson, J.M., Schmeeckle, M.W., Shreve, R.L., McLean, S.R. (2001). Sediment Entrainment and Transport in Complex Flows. In: Seminara, G., Blondeaux, P. (eds) River, Coastal and Estuarine Morphodynamics. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-04571-8_2
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DOI: https://doi.org/10.1007/978-3-662-04571-8_2
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