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• W2004332897 abstract "The vertical distribution of the concentration of suspended particles is usually determined by solving the diffusion-convection equation under appropriate boundary conditions. The exponent in the resulting Rouse equation is the Rouse number, defined as z′ = vss /κu. The -value has been subject of much research, being ⋛ 1. This study focuses on the experimental determination of the depth-averaged -value, given by the ratio of the sediment, ∊ s , and the momentum, ∊ m , diffusion coefficients. These coefficients were evaluated under laboratory conditions from measurements of instantaneous velocity and concentration profiles, obtained simultaneously by using a non-intrusive sonar instrument, the Acoustic Particle Flux Profiler (APFP). In suspension flows over a movable bed without bed forms the measured -values at capacity condition are smaller than unity, < 1. However, it could also be shown that for flows over a movable bed with bed forms the -values are larger than unity, > 1; this is notably the case in natural waterways." @default.
• W2004332897 created "2016-06-24" @default.
• W2004332897 creator A5055054937 @default.
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• W2004332897 date "2002-07-01" @default.
• W2004332897 modified "2023-10-09" @default.
• W2004332897 title "Suspension flows in open channels; experimental study" @default.
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• W2004332897 doi "https://doi.org/10.1080/00221680209499886" @default.
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