HYDROGEOLOGY OF A FORESTED HEADWATER WETLAND ON THE SOUTHERN MARGIN OF THE LAKE ERIE DRAINAGE BASIN
Within 10m of the pond perimeter, a group of three 2.5cm PVC screened monitoring wells were installed at each of the four cardinal points of the compass: a shallow (40cm) soil-profile well, a deep (80cm) glacial-till well and a combination (85cm) well. A water-level gauge was installed in the pond. The wells were designed to monitor the water table within the soil profile (~0.3m thick) and/or underlying glacial tills (>10m thick) using the tape-&-chalk method. Climatological data were collected from a weather station located 1200m from the site. Site topography was mapped using a Sokkia Set 610 Total Station and Carlson Explorer data collector, supplemented with LIDAR data.
Preliminary results suggest that the pond and wetland constitute a recharge system ~90% of the time with groundwater flowing from the pond-wetland out into the surrounding deciduous forest. Through-flow conditions were not observed. Following major rain events (>5cm/day), the groundwater flow direction reverses and the pond-wetland becomes a discharge system for up to several days. Precipitation-water table comparisons suggest an Sy of ~10% for the glacial till. The water table beneath the largest two of five catchment sub-basins responds rapidly (1-2day) and dramatically (60-80cm) to heavy (8cm/day) rainfall events.