This paper describes a model of the diffusive boundary-layer around an
aquatic macrophyte blade. Nutrient uptake at the base of the modelled
boundary-layer was examined using previously published laboratory dat
a. The analysis showed that, over the outer velocity range 0.01-0.16 m
s(-1), nutrient uptake varied between that predicted by flat plate bou
ndary-layer theory and that expected with no mean advection. A ratio o
f theoretical and actual nutrient uptake rates was defined as a means
of categorising the transition between the two transport models. The m
odelling was extended to show how fluctuating boundary conditions may
enhance nutrient uptake by the macrophyte; the scenario examined here
suggested that at otherwise low outer velocities, periodic stripping o
f the boundary-layer by passing waves increased nutrient uptake by a f
actor of 10.