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Groundwater vulnerability to herbicides varies throughout the wheat-growing regions across the nation. Groundwater Vulnerability in Wheat-Growing Variability is a function of soil types, weather patterns, depth to ground water, and wheat cultivation Regions of the United States practices. National datasets including the Soil Survey Geographic (SSURGO) database and Cropland Data Layer (CDL) can be used in conjunction with groundwater models to capture the range in vulnerability.

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Less than 4 to 20 Greater than Exposure Calculation 4 meters meters 20 meters Groundwater Modeling The map at left shows, at the county level, the Aquifer Depth relative exposure to groundwater from an Groundwater modeling was conducted throughout the nation herbicide applied to wheat. Exposure scores are Although groundwater modeling was conducted with a constant aquifer depth of 4 with the Pesticide Root Zone Model (PRZM) for unique the product of county-average model-predicted meters from the surface, the shallow aquifer depth in wheat-growing regions varies combinations of soil types, weather patterns, and wheat herbicide concentrations in the shallow aquifer widely throughout the United States. Predicted groundwater herbicide cultivation practices assuming a shallow aquifer depth of 4 and the fraction of the county growing wheat. concentrations are sensitive to the aquifer depth. Deeper aquifers generally have meters. Model-predicted concentrations of an herbicide in the Low exposure counties are shown as lighter lower exposure to herbicides via movement through the soil profile over a given shallow aquifer varied throughout each county. To illustrate the and higher exposure counties are shown as time period. Groundwater depth data from wells ( dots at left) in the Principal variability, locations of wheat fields and their corresponding darker red. To standardize the basis of Aquifers of the United States (USGS) were used to identify more vulnerable concentrations are shown at left for parts of Colorado, Kansas, comparison, all counties are assumed to have 2 locations for subsequent analysis. The Principal Aquifers are mapped at left and 1 New Mexico, Texas, and Oaklahoma. Lower to higher the same depth to shallow aquifer (4 meters). concentrations are symbolized from to . above.

Lauren Padilla1, Mike Winchell1, Natalia Peranginangin2, Shanique Grant2, Charlie Hoffman1, Katie Budreski1 1. Stone Environmental 2. Syngenta Crop Protection

For more information about groundwater modeling and vulnerability contact Lauren Padilla at Stone Environmental, [email protected]