PREDICTING ARSENIC IN DRINKING WATER WELLS IN GLACIAL AQUIFERS IN WESTERN AND CENTRAL MINNESOTA, USA
A Boosted Regression Tree (BRT) model was developed to predict the probability of elevated arsenic in groundwater at typical drinking water supply depths in glacial aquifers in western and central Minnesota. Predictive factors used to build the BRT model were obtained from a variety of existing data sets and consisted of about 75 different factors such as well construction, and glacial aquifer/surficial (e.g. soil texture, soil chemistry, land use) characteristics. The final BRT model predicted the probabilities of elevated arsenic in groundwater with about 65% accuracy. Predictive factors determined to be important for predicted probabilities included clay gap (distance from top of screen to overlying confining unit), nearest major river (a proxy for hydrological position in the landscape), horizontal hydraulic conductivity, and distance to the top of the bedrock from the bottom of the well. For example, smaller clay gaps were typically related to higher probability of elevated arsenic concentrations. This is the first successful application of BRT to model probabilities of elevated arsenic in a complex glacial aquifer system. The BRT model was used to generate maps illustrating probabilities of elevated arsenic across the modeled regions at the depth and with the construction characteristics typical of drinking water wells. The BRT model could be used to create a 3-D tool to reduce the risk of drilling wells with elevated arsenic.