U.S. Geological Survey Toxic Substances Hydrology Program--Proceedings
of the Technical Meeting, Colorado Springs, Colorado, September 20-24, 1993,
Water-Resources Investigations Report 94-4015
 
Fate of Alachlor, Atrazine, and Bromide in a Corn Plot near
Topeka, Kansas
by
D.A. Eckhardt (U.S. Geological Survey, Ithaca, NY), R.J. Wagenet
(Cornell University, Ithaca, NY), E.M. Thurman (U.S. Geological Survey,
Lawrence, KS), and P.L. Barnes (Kansas State University, Manhattan, KS)
Abstract
In April 1991, a bromide tracer and the herbicides atrazine and alachlor
were applied to a 0.75-hectare (ha) field plot of Eudora silt loam in the
Kansas River Valley near Topeka, Kansas. The chemicals were immediately
disked into the top 7.5 cm of soil, and the plot was planted with corn.
Composite soil cores were collected from 12 contiguous cells in the plot,
each 15 meters (m) by 15 m, at 15-centimeter (cm) depth intervals to 90
cm. Cores were collected immediately after application, then after 30, 60,
and 120 days. Mean atrazine losses from the soil profile, relative to the
immediate postapplication core results, were 75 percent at day 30, 92 percent
at day 60, and 96 percent at day 120. Mean alachlor losses were 93 percent
at day 30, 99 percent at day 60, and nearly 100 percent by day 120. The
ratio of desethylatrazine metabolite to atrazine concentrations steadily
increased in the top 15-cm soil layer during the 120-day period. An analysis
of the soil-water budget and bromide distribution in the soil profile indicates
that downward movement of the chemicals was restricted by a lack of significant
downward soil-water flux during the growing season, when evapotranspiration
was greatest. Loss of the herbicides from the soil profile is attributed
mainly to degradation and transformation, and loss of bromide is attributed
mainly to uptake by the crop. Low but persistent herbicide concentrations
120 days after application indicate that herbicide half lives are not constant
and that herbicide residues could be tightly bound within solid-phase organic
carbon and unavailable for biotic degradation.
 
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