The ultimate fate of inorganic phosphorus in natural waters is to a large d
egree determined by interactions with sediments. The interactions in river
bed sediments have been investigated by a combination of methods using surf
ace sediments, <2 mm in diameter, collected from a 55 km stretch of the Riv
er Swale in Yorkshire, UK. The sediments were analysed by digestion (Fe, Ca
and P), clay mineralogy and their equilibrium phosphate concentration. All
the equilibrium phosphate concentrations were below 2 mu mol dm(-3), which
is much less than the concentration in the overlying water and indicates a
net uptake of phosphorus by the sediments. Experiments in a fluvarium chan
nel with a coarse sediment also showed that the release and uptake of solub
le phosphorus was towards a steady-state concentration in the overlying sol
ution, consistent with measurements of the equilibrium phosphate concentrat
ion. A kinetic model describing the net uptake of soluble reactive phosphor
us by river sediments was applied to chemical data collected during an inte
nsive monitoring exercise in the catchment. Copyright (C) 1999 John Wiley &
Sons, Ltd.