Results are reported on detailed measurements of suspended sediment concent
ration and particle size profiles, collected using a multi-frequency acoust
ic backscatter system in the river Taw estuary, UK, over a sandy rippled be
d. The acoustic data were augmented with electromagnetic and rotary current
meter measurements of the flow and in situ pumped samples of the suspended
sediments. Combining the conventional flow and pumped sampled measurements
with the high-resolution multi-frequency acoustic data, an examination of
sediment diffusivity profiles, reference concentrations and mean suspended
sediment concentration profiles has been conducted. Utilising the high vert
ical spatial resolution of the acoustic system, profiles of the sediment co
ncentration and sediment diffusivity have been used to obtain beta the rati
o of sediment diffusivity to eddy viscosity. These results show beta to be
independent of the height above the bed, with consistent values typically i
n the range beta t approximate to 1-2. A new empirical expression has been
formulated for fl using available tidal field data. Employing the capabilit
y of acoustics to obtain unobtrusive very near-bed concentration measuremen
ts, estimates for the reference concentration based on the van Rijn (J. Hyd
raulic Engng 110 (11) (1984) 1613) definition have been obtained. The measu
rements are compared with predictions and the results show that the predict
ions are typically within a factor of two of the measurements. Finally usin
g the sediment diffusivity results, a two-layer representation for the mean
suspended sediment concentration profile is suggested. This representation
has been used to generate suspended sediment concentration profiles and th
ese are shown to be in good agreement with the measured profile. (C) 2001 E
lsevier Science Ltd. All rights reserved.