A set of experiments was carried out to determine what effects periphy
ton communities could have on near-bed hydraulic fields. We analysed v
elocity distribution, skewness and kurtosis coefficients, Reynolds str
esses, relative turbulence intensity, coefficient of eddy diffusivity,
Velocity spectra, and turbulence scales at two flows with, and withou
t, diatom-dominated periphyton on the bed. We found that turbulence wa
s affected by the periphyton mat selectively. The largest influence oc
curred for the velocity distribution, Reynolds stress, coefficient of
eddy diffusivity, and velocity cross-spectra. Changes as a result of t
he periphyton mat were revealed in the large-scale turbulence structur
e. The periphyton affected not only the region near the bottom but als
o the entire logarithmic layer. The periphyton mat increased roughness
length by a factor of approximate to 5 whereas the integral resistanc
e to flow (reciprocal Chezy coefficient and Manning's roughness coeffi
cient) was increased by 20-25%. The microscale turbulence structure wa
s investigated using values of Kolmogorov's microscale eta(K). These a
ppeared to be commensurate with the characteristic scales of periphyto
n filaments. This allowed us to hypothesise that the mechanism of the
''periphyton-turbulence'' interaction is connected, to a certain degre
e, with viscous effects.