Rd. Smith et al., EFFECTS OF EXPERIMENTAL REMOVAL OF WOODY DEBRIS ON THE CHANNEL MORPHOLOGY OF A FOREST, GRAVEL-BED STREAM, Journal of hydrology, 152(1-4), 1993, pp. 153-178
Experimental removal of woody debris from a small, gravel-bed stream i
n a forested basin resulted in dramatic redistribution of bed sediment
and changes in bed topography. Removal of debris changed the primary
flow path, thereby altering the size and location of bars and pools an
d causing local bank erosion and channel widening. Marked bed adjustme
nts occurred almost immediately following experimental treatment in Ma
y 1987 and continued through to the end of the study period in 1991. I
ncreased bed material mobility was attributable to destabilization of
sediment storage sites by removal of debris but-tresses, elimination o
f low-energy, backwater environments related to debris, and an inferre
d increase in boundary shear stress resulting from the removal of debr
is-related flow resistance. In contrast to these changes, which favore
d sediment mobilization, deposition was favored by the elimination of
debris-related scouring turbulence and by increased flow resistance fr
om a developing sequence of alternate bars. A more regularly spaced se
quence of alternate bars replaced the pretreatment bar sequence, whose
location, size, and shape had been strongly influenced by large woody
debris as well as by bank projections and channel curvature. Followin
g initial readjustment of the stream bed during the first posttreatmen
t year, loss of scouring turbulence and increased flow resistance from
alternate bars resulted in deposition of approximately 44 m3 of sedim
ent within the 96 m study reach. The loss of 5.2 m3 to bank erosion le
ft a net increase in sediment storage of 39 m3. Mean spacing of thalwe
g cross-overs and pools did not change measurably following debris rem
oval, although variability of spacing between thalweg cross-overs tend
ed to decrease with time as the location of bars stabilized. No consis
tent pattern of change in mean residual depth of pools or in distribut
ion of depths occurred within the first 4 years following debris remov
al.