EVOLVING CONCEPTUAL HYDROGEOLOGIC MODELS FOR COMPLEX GLACIAL AQUIFER SYSTEMS
At the Pall Life Sciences site, wastewater containing 1,4-dioxane was discharged into unlined seepage lagoons and spray irrigated across a 15 acre field from 1967 to 1985. Plumes of 1,4-dioxane-contaminated groundwater have migrated several kilometers from the site in different directions through the underlying 80m of glacial drift. Because 1,4-dioxane is readily soluble in water and does not easily degrade or adsorb to soil particles, it provides a tracer-like record of solute transport. More than 120 monitoring wells and 16 extraction wells have been drilled to investigate and remediate 1,4-dioxane in the area. In spite of attempts to contain and remove the contaminant following its discovery two decades ago, remediation activities have met with limited success; and efforts to characterize and model the aquifer continue as the deepest known plume advances toward a municipal water supply well and the Huron River. Analysis of the Pall Life Sciences dataset suggests that the utilization of geostatistics within a deterministic sequence stratigraphic framework and the application of GIS tools to subsurface investigations will improve our ability to model and predict contaminant transport in complex glacial aquifer systems.