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Detailed Reference Information |
Gratiot, N., Michallet, H. and Mory, M. (2005). On the determination of the settling flux of cohesive sediments in a turbulent fluid. Journal of Geophysical Research 110. doi: 10.1029/2004JC002732. issn: 0148-0227. |
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In this paper we compare the settling flux of a cohesive sediment mixture measured in a quiescent fluid with that achieved in a turbulent flow. Experiments were performed in a mixing tank. The turbulence produced mechanically by an oscillating grid maintains a stationary, highly concentrated fluid mud layer in which the concentration is almost uniform. In this layer the turbulence decay with increasing distance from the grid is similar to that obtained in clear water. For steady conditions the settling flux of the fluid mud mixture is balanced by the upward turbulent flux, and its value can be determined from the measured depth of the fluid mud layer. At high concentrations (10--200 g L-1), we show that the settling flux in a turbulent fluid is much larger than estimated in a quiescent fluid (up to two orders of magnitude). Hindering effects in the settling process of cohesive sediments may thus be considerably reduced by turbulence. |
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Abstract |
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Keywords
Oceanography, Physical, Sediment transport, Oceanography, Physical, Turbulence, diffusion, and mixing processes, Oceanography, Physical, Instruments and techniques, Marine Geology and Geophysics, Marine sediments, processes and transport, Oceanography, General, Estuarine processes, hindered settling, fluid mud, lutocline, stratified flows, turbulent diffusion, oscillating grid experiments |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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