Flume studies showed that narrow hedges of tall, stiff grasses across
locations of concentrated overland flow have great potential for retar
ding runoff and reducing sediment losses. Hedges of switchgrass and ve
tiver caused backwater depths of up to 400 mm and trapped more than 90
% of sediment coarser than 125 mu m. Lesser percentages were trapped a
s sediment size decreased, with only about 20% of the material finer t
han 32 mu m caught. Sediment trapping resulted mostly from upslope pen
ding by the hedges rather by filtering action, so the physical charact
eristics of the different grasses were important primarily to the exte
nt that they retarded flow.