K. Black et A. Cramp, A DEVICE TO EXAMINE THE IN-SITU RESPONSE OF INTERTIDAL COHESIVE SEDIMENT DEPOSITS TO FLUID SHEAR, Continental shelf research, 15(15), 1995, pp. 1945-1954
A self-contained, field-portable recirculating seawater flume was desi
gned and constructed in order to measure in situ the erodibility of co
hesive estuarine muds. The flume can be easily deployed by one person
and is designed for subaerial use only. Bed shear stresses up to 0.6 N
m(-2) can be generated by the flume. Rates of sediment erosion are ass
essed in terms of the mass of particulate material eroded with time. F
low calibrations yield a drag coefficient (C-D) of 4.5 x 10(-3) which
enables single mid-depth velocity measurements to be related directly
to the imposed bed stress. Water motions within the flume are complex,
but secondary (radial) circulations are not considered sufficiently c
ompetent to dominate sediment erosion. Stratification effects due to h
igh levels of suspended sediment (similar to 1.5 gl(-1)) are negligibl
e. However, the drag-reducing properties of the sediment suspension ar
e uncertain.