CBS layers in a diffusive turbulence grid oscillation experiment

M Mory, N Gratiot, AJ Manning, H Michallet

Research output: Chapter in Book/Report/Conference proceedingChapterpeer-review

Abstract

The generation of a Concentrated Benthic Suspension (CBS) of a fluid mud mixture is investigated in the laboratory in a grid stirred experiment. A sediment concentration in the CBS layer in the range 3 g/l to 200 g/l was considered. The sediment concentration, the turbulence properties, and the settling velocity have been measured. The decay of turbulence with increasing distance from the grid is not found to vary with the concentration inside the CBS layer except in the vicinity of the lutocline. The settling velocity decreases rapidely with increasing sediment concentration and appears to be the most sensitive parameter in the experiment. A clear difference in the value of the flux Richardson number at the lutocline is observed depending on the sediment concentration. Rif is about 0.1 for the highest concentrations and increases above 0.5 for the low concentration cases.
Original languageEnglish
Title of host publicationFine Sediment Dynamics in the Marine Environment - Proc. in Marine Science 5
EditorsJC Winterwerp, C Kranenburg
PublisherElsevier Science
Pages139-154
Number of pages15
Volume5
Publication statusPublished - 1 Jan 2002

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