GSA Connects 2023 Meeting in Pittsburgh, Pennsylvania

Paper No. 156-6
Presentation Time: 9:20 AM

THREATS TO GROUNDWATER RESOURCES IN THE CHEQUAMEGON-NICOLET NATIONAL FOREST, WISCONSIN


SWANSON, Susan1, GRAHAM, Grace1, CHASE, Pete1, FEHLING, Anna2 and PRUITT, Aaron2, (1)Wisconsin Geological and Natural History Survey, University of Wisconsin-Madison, Madison, WI 53705, (2)Wisconsin Dept. of Natural Resources, Madison, WI 53703

The Chequamegon-Nicolet National Forest (CNNF) in northern Wisconsin contains numerous groundwater-dependent water resources that may be vulnerable to potential effects of land development, mining, and climate change. Recent work inventoried groundwater resources in the four units of the CNNF (Park Falls, Medford, Nicolet, Washburn/Great Divide) and developed tools to improve the understanding of aquifer characteristics and groundwater flow. Several new studies are further characterizing water chemistry across the CNNF; establishing baseline hydrogeologic conditions near the Bend Copper-Gold Deposit, a potentially viable deposit for mining; and investigating the vulnerability of seepage lakes to groundwater flooding. To assess water quality conditions, samples from over 160 lakes, streams, and wells were analyzed for major ion chemistry in 2016 and again in 2021-22. Throughout the national forest, mostly non-carbonate unlithified glacial deposits overlie crystalline bedrock. As a result, concentrations of most ions in groundwater and surface waters are relatively low. Locally, elevated chloride suggests some influence from road salting. However, water quality in all four units of the CNNF is very good and considered pristine in many areas, thus highlighting its vulnerability to human activities in the future. For the many seepage lakes and wetlands in the region, projected changes in the amount of precipitation and the frequency of extreme events brings flooding concerns from rising groundwater and threats to groundwater-dependent habitats. The subtle glacial topography of the region and variations in the elevation of the bedrock surface can lead to differences between surface flows and groundwater movement further complicating the prediction of these often prolonged events. These examples underscore the contributions of the previous forest-wide inventories and the need for ongoing work to address the full range of future challenges to the water resources of the CNNF.