In the research presented here, we examine the effects of water velocity an
d canopy morphology on rates of nutrient uptake by seagrass communities. Am
monium uptake rates for two types of seagrass communities, Halodule wrighti
i and Thalassia testudinum, are measured over a range of velocity using a f
ield flume. The field flume allows independent measurements of uptake by co
mmunities of natural composition and condition. We compare our results with
those estimated using empirically derived engineering equations that descr
ibe transport processes to rough surfaces in order to explore the possibili
ty that uptake rates can be predicted from these equations. We also investi
gate the possibility that the seagrass canopy alters the characteristics of
water flow within the community, which is reflected by the friction impose
d by the canopy (the friction coefficient) on the moving water. Our results
indicate that ammonium uptake by seagrass communities is dependent on wate
r velocity. Further, seagrasses affect characteristics of water flow within
the community that are reflected in rates of ammonium uptake. Empirically
derived engineering equations used with measured friction coefficients yiel
d expected Stanton numbers (a nondimensional ratio of flux to a surface to
advection by a surface) that are within 95% of those measured in the field
flume. Thus, the capacity of these communities to remove ammonium from the
water column can be predicted using empirically derived engineering equatio
ns that describe the transport of chemicals between a fluid and a rough sur
face.