Detailed velocity measurements made with laser Doppler velocimetry hav
e shown that, except very close to the bed, the production of turbulen
ce within a stand of emergent vegetation is dominated by the stem wake
s rather than by the bottom-boundary shear, as in open-channel flows.
This observation formed the basis for a modified random-walk model tha
t describes the contribution of stem wakes to the turbulent diffusivit
y within marsh passes. The model was validated by comparison to observ
ed diffusivity over a range of population and flow conditions within a
simple plantlike array of circular cylinders. The diffusion model was
also evaluated for a more complex morphology that included a flexible
canopy. Laser-induced fluorescence and image-processing techniques we
re used to measure the diffusivity as well as to examine turbulence st
ructure within the experimental system. The latter analysis documented
changes in turbulence scale that arise as larger eddies are broken ap
art by the stems and smaller eddies (comparable to the stem diameter)
are produced within the wakes.