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Observed and predicted vertical suspended sediment concentration profiles and bedforms in oscillatory-only flow Williams, J.J.; Bell, P.S.; Thorne, P.D.; Trouw, K.; Hardcastle, P.J.; Humphrey, J.D. (2000). Observed and predicted vertical suspended sediment concentration profiles and bedforms in oscillatory-only flow. J. Coast. Res. 16(3): 698-708 In: Journal of Coastal Research. Coastal Education and Research Foundation: Fort Lauderdale. ISSN 0749-0208; e-ISSN 1551-5036, meer

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Beschikbaar in	Auteurs
VLIZ: Open Marine Archive 232429 [ download pdf ] Waterbouwkundig Laboratorium: Overdrukjes 152261 [ aanvragen ]

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Trefwoorden

Flow Flow Layers > Boundary layers > Benthic boundary layer Model studies Movement > Flow Oscillatory flow Particulates > Suspended particulate matter > Sediments > Resuspended sediments Physics > Mechanics > Dynamics > Sediment dynamics Profiles > Vertical profiles Sediments > Clastics > Sand Waves Waves Marien/Kust

Author keywords

deltaflume; pump-sampling; hydraulic roughness; diffusion; vortex; diffusivity; wave mixing; acoustic bed imaging

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Auteurs		Top
Williams, J.J. Bell, P.S. Thorne, P.D.	Trouw, K., meer Hardcastle, P.J. Humphrey, J.D.

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Abstract

Measurements of hydrodynamic conditions and vertical suspended sediment concentration profiles, C-profiles, have been obtained above rippled sandy beds in a large wave flume. Measured values of wave height and period, water depth and sediment properties are used in well-known formulae to predict sediment dynamics and bed shear stresses due to waves. These data are then used in an existing convective model and a new model to predict C-profiles. Measured C-profiles and C-profiles predicted by the new model are shown to agree well for a range of grain sizes and wave conditions. Grain-scale bed roughness, defined using data from the model, is found to vary with the wave mobility number. Values for the wave mixing coefficient derived using the new model are tested and are found to agree well with published values and with theory.

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