The functional relationships between rainfall intensities and amounts,
and the washoff of dicamba and 3,6-DCSA from turfgrass foliage were d
etermined. Dicamba was applied to Kentucky bluegrass field plots and t
he turfgrass was subjected to 2 to 58 mm of simulated rainfall 18 to 4
8 h later. Rainfall was applied at an average intensity of 20.6 or 39.
9 mm h-1. The 39.9 mm h-1 intensity reduced dicamba washoff by 10% for
a given amount of rainfall. Washoff of 3,6-DCSA was independent of ra
infall intensity. When averaged over intensities, washoff of dicamba w
as best described by the equation y = 1 - 0.341X0.187, and 3,6-DCSA wa
shoff by the equation y = exp(-0.210x), where x represents millimeters
of rainfall and y, the proportion of compound remaining on the foliag
e after rainfall.