Joint 72nd Annual Southeastern/ 58th Annual Northeastern Section Meeting - 2023

Paper No. 2-6
Presentation Time: 10:00 AM

USE OF FALLOUT RADIONUCLIDES TO ASSESS FIELD-TO-GAUGE CONNECTIVITY IN GREAT LAKES RESTORATION INITIATIVE PRIORITY WATERSHEDS


KARWAN, Diana1, HANKINS, Ryan1, PAWLOWSKI, Ethan2, WILLIAMSON, Tanja3, ROSE, Lucy4, KOLKA, Randy5 and FITZPATRICK, Faith6, (1)Department of Forest Resources, University of Minnesota, 301G Green Hall, 1530 Cleveland Avenue North, St. Paul, MN 55108, (2)University of Minnesota–Twin Cities, (3)USGS, OH-KY-IN Water Science Center, Louisville, KY 40018, (4)Department of Forest Resources, University of Minnesota–Twin Cities, (5)USDA Forest Service - Northern Research Station, Center for Research on Ecosystem Change, 1831 Hwy. 169 E, Grand Rapids, MN 55744, (6)U. S. Geological Survey, 8505 Research Way, Middleton, WI 53562

Short-term fallout radionuclides, Beryllium-7 (7Be) and excess Lead-210 (210Pbxs) were used to elucidate the contribution of in-channel transport and biogeochemical processing of sediment and associated phosphorus transport from field to watershed outlets in priority watersheds of the Great Lakes Restoration Initiative. Multiple collections took place in Plum Creek (Fox River Basin) and Black Creek (Maumee Basin). Seasonal storm data has been collected over the 2018-2019 seasons at edge-of-field sites in both watersheds. Throughout the 2019 growing season, suspended sediments were sampled from three nested in-stream locations in Plum Creek. Initial Plum Creek results show higher 7Be/210Pbxs ratio with downstream position, which we interpret as increased 7Be and 210Pbxs sorption to sediments within the wider, downstream portion of the channel. Follow up work will be done to assess the influence of sediment specific surface area on these results. At the Black Creek site, 7Be activity was measured in contributing waters to Black Creek, surface water runoff and tile drain effluent from two paired, adjacent fields during eleven events. Tile drain waters carried detectable 7Be, indicating event-timescale hydrologic transport to and through the tile network. For one tile, the 7Be activity was similar in activity to the surface runoff. For the second tile, 7Be was much lower while other chemical tracers of groundwater (e.g. nitrate/nitrite) were much higher, indicating a higher water table. In both studies, 7Be has been a useful tracer to discern connectivity on an event to seasonal timescale.