Herbicides are detected in rainfall; however, these are a small fracti
on of the total applied. This study was designed to evaluate monthly a
nd annual variation in atrazine hyl-N'-(1-methylethyl)-1,3,5-triazine-
2,4-diamine) alachlor o-N-(2,6-diethylphenyl)-N-(methoxymethyl)acetami
de metolachlor thylphenyl)-N-(2-methoxy-1-methylethyl)acetamide), and
NO3-N concentrations in rainfall over Walnut Creek watershed south of
Ames, IA. The study began in 1991 and continued through 1994. Within t
he watershed, two wet/dry precipitation samplers were positioned 4 km
apart. Detections varied during the year with >90% of the herbicide de
tections occurring in April through early July. Concentrations varied
among events from nondetectable amounts to concentrations of 154 mu g
L(-1), which occurred when atrazlne was applied during an extremely hu
mid day immediately followed by rainfall of <10 mm that washed spray d
rift from the atmosphere. This was a local scale phenomenon, because t
he other collector had a more typical concentration of 1.7 mu g L(-1)
with an 8-mm rainfall. Variation between the two collectors suggests t
hat local scale meteorological processes affect herbicide movement. Ye
arly atrazine deposition totals were >100 mu g m(-2) representing <0.1
% of the amount applied. Nitrate-N concentrations in precipitation wer
e uniformly distributed throughout the year and without annual variati
on in the concentrations. Deposition rates of NO3-N were about 1.2 g m
(-2). Annual loading onto the watershed was about 25% of the amount ap
plied from all forms of N fertilizers. Movement and rates of depositio
n provide an understanding of the processes and magnitude of the impac
t of agriculture on the environment.