Convective Sedimentation from a Stable Turbid Layerby Theodore Green, Univ of Wisconsin, United States,
El Sayed Mogahed, Univ of Wisconsin, United States,
Document Type: Proceeding Paper
Part of: Sediment Transport Modeling
A set of experiments was conducted to test T Green's criterion for the existence of double-diffusive convective motions at an originally sharp, horizontal interface separating upper, less-dense turbid water from lower, more-dense clear water. The results are discussed.
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