A unique flume that measures the erosion of sediments at high shear st
resses and with sediment depth has been designed, constructed, and use
d. Experiments in this flume, Sedflume, can be done either with recons
tructed sediments or with relatively undisturbed sediments from the fi
eld. With either kind of sediment, two different types of experiments
can be conducted. The first type determines the critical stress for er
osion of the sediment as a function of depth, while the second type de
termines the erosion rate of the sediment as a function of both shear
stress and depth. Measurements of the erosion rates of sediments from
the Trenton Channel of the Detroit River in Michigan and the Lower Fox
Fiver in Wisconsin were made by use of Sedflume at sediment depths up
to 2 m. Representative results of these measurements are presented he
re. These results demonstrate the capabilities of Sedflume and also il
lustrate the large differences in erosion rates at different sites and
the large variations in erosion rates with depth and as a function of
shear stress.