Glyphosate use in a watershed results in some occurrence in surface water; however, the watersheds most at risk for the offsite transport of glyphosate are those with high application rates, rainfall that results in overland runoff and a flow route that does not include transport through the soil.
Water samples were collected from 88 municipal wells
throughout Iowa during the summer and were collected
monthly at 12 stream sites in eastern Iowa from March
to December 1996 to study the occurrence of the sulfonic
and oxanilic metabolites of acetochlor, alachlor, and
metolachlor. The sulfonic and oxanilic metabolites
were
present in almost 75% of the groundwater samples and
were generally present from 3 to 45 times more frequently
than their parent compounds. In groundwater, the
median
value of the summed concentrations of acetochlor,
alachlor, and metolachlor was less than 0.05 μg/L, and
the median value of the summed concentrations of the six
metabolites was 1.2 μg/L. All surface water samples
contained at least one detectable metabolite compound.
Individual metabolites were detected from 2 to over
100
times more frequently than the parent compounds. In
surface
water, the median value of the summed concentrations
of the three parent compounds was 0.13 μg/L, and the
median
value of the summed concentrations of the six metabolites
was 6.4 μg/L. These data demonstrate the importance
of
analyzing both parent compounds and metabolites to
more fully understand the environmental fate and transport
of herbicides in the hydrologic system.
Herbicide compounds were prevalent in ground water across Iowa, being detected in 70% of the 106 municipal wells sampled during the summer of 1995. Herbicide degradation products were three of the four most frequently detected compounds for this study. The degradation product alachlor ethanesulfonic acid was the most frequently detected compound (65.1%), followed by atrazine (40.6%), and the degradation products deethylatrazine (34.9%), and cyanazine amide (19.8%). The corn herbicide acetochlor, first registered for widespread use in the United States in March 1994, was detected in a single water sample. No reported herbicide compound concentrations for this study exceeded currem U.S. Environmental Protection Agency's maximum contaminant levels or health advisory levels for drinking water, although the herbicide degradation products examined have yet to have such levels established.
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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