Vi. Nikora et al., THE EFFECTS OF THE MOSS FISSIDENS RIGIDULUS (FISSIDENTACEAE, MUSCI) ON NEAR-BED FLOW STRUCTURE IN AN EXPERIMENTAL COBBLE BED FLUME, Limnology and oceanography, 43(6), 1998, pp. 1321-1331
The effects of the aquatic moss Fissidens rigidulus on near-bed flow s
tructure in a cobble-lined flume were investigated. Moss-covered cobbl
es were placed in the flume, and velocities were measured at six verti
cal profiles upstream, above, and downstream of the cobbles. All measu
rements were replicated at three different discharges. An acoustic dop
pler velocimeter (ADV) was used to measure velocity fluctuations in th
ree dimensions at each point, at a 0.04-s sampling interval for 2 min.
Following this, the moss was removed without disturbing the cobbles'
spatial arrangement, and measurements were repeated to characterize ba
ckground hydraulic conditions. We investigated mean local velocities,
Reynolds stresses, total turbulence energy, relative turbulence intens
ities, and velocity spectra with and without the moss. Two how layers
were observed in all our experiments: an upper logarithmic layer and a
lower roughness sublayer. Velocities in the upper layer followed the
standard logarithmic law, whereas velocities in the roughness sublayer
did not, because of interaction between flow and the roughness elemen
ts. The presence of Fissidens caused a reduction in average longitudin
al velocity, Reynolds stress, and total turbulence energy. Relative tu
rbulence intensity was much higher in the presence of the moss. An int
ernal boundary layer (IBL) around the moss was also observed; this IBL
was destroyed behind the moss by turbulent mixing in the roughness su
blayer. The IBL thickness increased with increasing flow.