Large woody debris (LWD) are the logs, sticks, branches, and otherwood that falls intostreams andrivers. This debris can influence theflow and the shape of the stream channel. Large woody debris, grains, and the shape of the bed of the stream are the three main providers of flow resistance, and are thus a major influence on the shape of the stream channel.[1] Some stream channels have less LWD than they would naturally because of removal by watershed managers for flood control and aesthetic reasons.[2]
The study of woody debris is important for itsforestry management implications. Plantation thinning can reduce the potential for recruitment of LWD into proximal streams. The presence of large woody debris is important in the formation of pools which serve assalmon habitat in the Pacific Northwest.[3] Entrainment of the large woody debris in a stream can also causeerosion and scouring around and under the LWD. The amount of scouring and erosion is determined by the ratio of the diameter of the piece, to the depth of the stream, and the embedding and orientation of the piece.[citation needed]
Large woody debris slows the flow through a bend in the stream, while accelerating flow in the constricted area downstream of the obstruction.[4]
