Titlebook: Sediment/Water Interactions; Proceedings of the F B. T. Hart,P. G. Sly Conference proceedings 1992 Springer Science+Business Media Dordrech

HUSH

Flocculation and its effect on the vertical transport of fine-grained sedimentswo orders of magnitude, than those predicted by mono-disperse theory. The model is also used to show that the disaggregation of flocs due to increased shear near the sediment-water interface may be a possible mechanism for the increased concentrations often observed near this interface.

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Flocculation and its effect on the vertical transport of fine-grained sedimentsionally efficient model of the aggregation and disaggregation of fine-grained sediments is proposed. This model is then used to predict flocculation times and steady-state floc sizes for a wide range of environmental conditions. The predicted flocculation times are smaller, sometimes by as much as t

掙扎

Transport and distribution of sediments along the Ligurian coast Varazze and Cape Noli (Ligurian Sea), provided useful information on transport and sedimentation processes in the area. Sediments samples from the shelf were highly heterogeneous, ranging from pelites to sands. Minerals typical of individual river basins were found close to river mouths, indicating

Frequency

格言

Storage, redistribution and net export of dissolved and sediment-bound nutrients, Vejle Fjord, Denmaources to Vejle Fjord during the period September 1988 to October 1989 is exported to the Kattegat. The sediment nutrient concentrations in the estuary are mainly governed by hydrography and resuspension. The general wind-induced circulation consists of outgoing currents along the southern side and

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OASIS

Wave-induced sediment resuspension in the ?re estuary, northern Swedenort of particles out of the estuary. Wave-induced sediment resuspension in the estuary was studied by monitoring the distribution of suspended particles during a resuspension-redeposition cycle. The particle concentration in the water mass was measured with a light scattering probe, calibrated by co

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Density

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