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    Author(s): Y. Cui; G. Parker; T. E. Lisle; J. Gott; M. E. Hansler; J. E. Pizzuto; N. E. Almendinger; J. M. Reed
    Date: 2003
    Source: Water Resources Research 39:1239, 1210.1029/2002WR001803.
    Publication Series: Miscellaneous Publication
    PDF: View PDF  (671 KB)


    Sediment often enters rivers in discrete pulses associated with landslides and debris flows. This is particularly so in the case of mountain streams. The topographic disturbance created on the bed of a stream by a single pulse must be gradually eliminated if the river is to maintain its morphological integrity. Two mechanisms for elimination have been identified: translation and dispersion.

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    Cui, Y.; Parker, G.; Lisle, T. E.; Gott, J.; Hansler, M. E.; Pizzuto, J. E.; Almendinger, N. E.; Reed, J. M. 2003. Sediment pulses in mountain rivers. Part 1. Experiments. Water Resources Research 39:1239, 1210.1029/2002WR001803.


    PSW4351, sediment, sediment pulse, landslides, debris flows, translation, dispersion, mountain rivers

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