The leaching behavior of agricultural chemicals depends on the applica
tion method of both the chemical and water. This study investigated th
e leaching behavior of conservative tracers under intermittent flood a
nd drip irrigation on a clay loam soil. Slug applications of conservat
ive tracers were applied sequentially to a single 37-m(2) plot and lea
ched under the two irrigation regimes with the same daily application
rate. Suction lysimeters, installed at seven depths (0.3, 0.6, 1.0, 1.
4, 1.8, 2.4, and 3.0 m) and replicated four times, were used to withdr
aw daily soil solution samples during leaching. Pore water velocities,
v, and dispersion coefficients, D, for a one-dimensional advection-di
spersion model were fit to the resulting concentration vs. time curves
by nonlinear least squares. Pore water velocities were slightly great
er on average under drip irrigation and were more uniform across the p
lot (smaller variance) than under flood irrigation. Preferential flow
was observed under both irrigation regimes. Breakthrough curves showed
considerably more spreading under intermittent flood irrigation than
under drip, indicating greater hydrodynamic dispersion under flood irr
igation. Fitted D values were, on average, nearly three times greater
under flood irrigation than under drip. Allowing free water at the soi
l surface during flood irrigation increased the dispersion of tracer c
ompared with the drip irrigation system, where water was applied at a
rate less than the saturated conductivity. The increase in D is most l
ikely due to small-scale spatial variability of the soil's hydraulic p
roperties.