In irrigated areas of Nebraska, agrichemical contamination of shallow
groundwater is characterized by much less areal variability than is co
mmonly associated with point-source contaminated areas. Existing high
capacity irrigation wells represent a cost-effective sampling network
for describing the areal extent of nonpoint-source contamination. Vari
ability in nitrate concentrations during pumping is important to both
the regulator and the farmer because the nitrate in the irrigation wat
er can meet some of the crop's N-requirement and the nitrate concentra
tion is an integral factor in preparing an accurate N-fertilizer budge
t, which may be mandated in Ground Water Quality Management and Specia
l Protection Areas. In order to ascertain the variability in the conce
ntrations of agrichemical contaminants during pumping, nitrate and atr
azine concentrations were measured in successive samples taken during
a 24-hour period from five high capacity irrigation wells located in h
eavily irrigated areas of Nebraska. In four of the wells stable analyt
e concentrations were attained in <0.25 hours after which fluctuations
in concentration hardly exceeded the analytical method variability. I
n established areas of nonpoint-source contamination with transmissive
formations, Papadopulos and Cooper's estimates for equilibration time
between the well and aquifer best approximate the actual time necessa
ry for the stabilization of these agrichemical concentrations in pumpe
d groundwater. The progressive decrease in the nitrate concentration d
uring the pumping of the fifth well reflects the radial variability in
analyte concentration in the aquifer around the well and correlates w
ell with land use, geology, and well design. In emerging areas of nonp
oint-source contamination with complex geology and short screened inte
rvals, longer pumping times may be necessary to attain uniform concent
rations.