Sediment deposition from flow at low gradients into a buffer strip--a critical test of re-entrainment theoryJournal of Hydrology, Vol. 280, No. 1-4. (September 2003), pp. 33-51.
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AbstractThe spatial and size distribution of sediment deposited from short periods of overland flow due to the effect of a simulated grass buffer strip was measured for low slopes of 1.6, 3.4 and 5.1%. These data were analysed so as to critically evaluate two alternative models of the process of re-entrainment of recently deposited sediment. A model of re-entrainment, previously thought to be appropriate only for a steady-state or equilibrium situation, was found to give better agreement with experiments than did a model previously used in the literature on this subject.
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