This paper describes a simple model for the desorption and transport of sol
uble reactive phosphorus (SRP) to subsurface drains. The model assumes firs
t-order kinetically rate-limited desorption in a soil surface mixing layer
over a soil profile layer that rests on an underlying, shallow restricting
layer. Input data include precipitation, soil hydraulic properties, drain o
utflow, free water surface fluctuation, sorbed P concentrations for the mix
ing layer and profile, desorption rate and equilibrium soil-SRP partitionin
g. Model results are compared to data on flow and SRP concentrations in dra
in outflow collected during natural rainfall events under field conditions.
The concentration time series simulated follow the sharp rise, peak, and g
radual recession of the observed field data. Predicted event mass loads res
ulting from observed and simulated tile discharges differ from the observed
load by +8.20% and -9.7%, respectively. Sensitivity analysis indicate that
equilibrium assumptions would not provide satisfactory results and that ma
ss transfer limits SRP release to the tile drain.