The migration of colloidal particles in the unsaturated zone may enhance le
aching of sorbing contaminants to surface waters and groundwaters. This pap
er describes a simple model of particle leaching and translocation based on
the dual-porosity model MACRO. The model includes descriptions of processe
s such as 'source-limited' particle detachment due to the kinetic energy of
rain, replenishment of the depleted store of particles up to a maximum val
ue determined by the amount of dispersible clay in the soil, and convective
transport of particles in macropores subject to a filter sink term varying
as a function of pore water velocity. Estimates of model parameter values
are obtained by comparing simulations with measurements of particle concent
rations in the discharge from tile drains made in a silty clay soil in sout
hwest Sweden. Calibrated in this way, the model is shown to reproduce satis
factorily the observations. A sensitivity analysis suggests that the critic
al parameters in the model are those related to particle filtering during v
ertical transport in soil macropores.