Statistical Properties of Sediment Movement

Statistical Properties of Sediment Movement

The downstream dispersion of a sediment bed particle is represented by a stationary point process in space and time domains and plausible forms of the probability density functions of the particle step length and rest duration are derived. The space rate parameter proposed in this paper gives step l...

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Veröffentlicht in:Journal of hydraulic engineering (New York, N.Y.) N.Y.), 1983-12, Vol.109 (12), p.1577-1588
Hauptverfasser: Cheong, Hin-Fatt, Shen, Hsieh-Wen
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container_issue 12
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container_title Journal of hydraulic engineering (New York, N.Y.)
container_volume 109
creator Cheong, Hin-Fatt
Shen, Hsieh-Wen
description The downstream dispersion of a sediment bed particle is represented by a stationary point process in space and time domains and plausible forms of the probability density functions of the particle step length and rest duration are derived. The space rate parameter proposed in this paper gives step length density functions whose forms vary from the exponential curve to the bell-shaped configuration. The time rate parameters used were proposed by Vukmirovic and Wilson. Theoretical results agree well with laboratory experimental data obtained for dune bed conditions.
doi_str_mv 10.1061/(ASCE)0733-9429(1983)109:12(1577)
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title Statistical Properties of Sediment Movement
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