
By 1Dana
W. Kolpin, 1Stephen
J. Kalkhoff, 2Donald
A. Goolsby, 1Debra
A. Sneck-Fahrer,
and 3E.
Michael Thurman
1U.S. Geological Survey, Iowa City, IA
2U.S. Geological Survey, Lakewood, CO
3U.S. Geological Survey, Lawrence, KS
The occurrence of herbicide compounds had a significant, inverse
relation to well depth and a significant, positive relation to dissolved-oxygen concentration. It is felt that both well depth and dissolved
oxygen are acting as rough surrogates to ground-water age, with younger ground water being more likely to contain
herbicide compounds. The occurrence of herbicide compounds was substantially
different among the major aquifer types across Iowa, being detected in 82.5% of
the alluvial, 81.8% of the bedrock/ karst region, 40.0% of the glacial-drift, and 25.0% of the bedrock/nonkarst region aquifers. The observed
distribution was partially attributed to variations in general ground-water age among these aquifer types. A significant, inverse relation was
determined between total herbicide compound concentrations in ground water and
the average soil slope within a 2-km radius of sampled wells. Steeper soil slopes may increase the
likelihood of surface runoff occurring rather than ground-water infiltration--decreasing the transport of herbicide compounds to ground water. As
expected, a significant positive relation was determined between intensity of
herbicide use and herbicide concentrations in ground water.
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