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.