Horizontal infiltration experiments were performed to validate a plug flow
model that minimizes the number of parameters that must be measured. Water
and silicone oil at three different viscosities were infiltrated into glass
beads, desert alluvium, and silica powder. Experiments were also performed
with negative inlet heads on air-dried silica powder, and with water and o
il infiltrating into initially water moist silica powder. Comparisons betwe
en the data and model were favorable in most cases, with predictions usuall
y within 40% of the measured data. The model is extended to a line source a
nd small areal source at the ground surface to analytically predict the sha
pe of two-dimensional wetting fronts. Furthermore, a plug how model for con
stant flux infiltration agrees well with field data and suggests that the p
roposed model for a constant-head boundary condition can be effectively use
d to predict wetting front movement at heterogeneous field sites if average
d parameter values are used.