The flow of a sediment layer that forms on an inclined plate as a cons
equence of the steady sedimentation of spherical particles was investi
gated theoretically as well as experimentally. The theoretical analysi
s was based on the model proposed by Nir and Acrivos (1990), modified
to include shear-induced diffusion due to gradients in the shear stres
s as well as a slip velocity along the wall due to the finite size of
the particles. The resulting set of partial differential equations, wh
ich is amenable to a similarity-type solution both near the leading ed
ge as well as far downstream, was solved numerically using a finite di
fference scheme thereby yielding theoretical predictions for the parti
cle concentration and velocity profiles, plus the local sediment layer
thickness, all along the plate. In addition, a new experimental techn
ique based on laser Doppler anemometry was developed and was used to m
easure the particle velocity profiles in the highly concentrated sedim
ent layer as well as the corresponding slip coefficient which relates
the slip velocity to the velocity gradient adjacent to a wall. The thi
ckness profile of the sediment layer was also measured experimentally
by means of video imaging. It was found that the experimental results
thus obtained for the particle velocity profile and for the local sedi
ment layer thickness were in very good agreement with the correspondin
g theoretical predictions especially considering that the latter did n
ot make use of any adjustable parameters.