Bromide (Br-) column leaching studies were conducted to estimate solut
e velocities and magnitude of preferential flow (ratio of solute to pi
ston flow velocities) under pending and high intensity sprinkler metho
ds. Twenty undisturbed Portneuf silt loam soil cores (250 mm x 300 mm)
were collected at spatially distributed locations in a 0.81-ha corn f
ield. The samples were divided into two sets of 10, and Br- leaching s
tudies were conducted under pending and high intensity sprinkler metho
ds. Analysis of the breakthrough curves (BTCs) indicated that preferen
tial flow occurred under both methods in all of the samples. The peak
and median solute velocities were 29-311% and 20-60%, respectively, la
rger than corresponding piston flow velocities. Though the solute velo
cities were larger under the pending method due to larger input flux v
alues, the average magnitude of the preferential flow was similar betw
een the two methods. The mobile-immobile model predicted the BTCs bett
er than the convection-dispersion model, with an average mobile percen
tage of 75 to 80. For the Portneuf silt-loam soil and given test condi
tions, the assumption of peak solute arrival to a given depth based on
piston flow is not valid because of large differences between the pea
k and piston flow velocities. The large variabilities measured for pea
k solute velocity under both methods indicate the importance of repeat
ed field measurements for determination of both magnitude and level of
uncertainty.