Field evaluation of arsenic transport across the groundwater/surface water interface: Groundwater discharge and iron oxide precipitation

GEOC 124

Robert G. Ford, ford.robert@epa.gov1, Kirk G. Scheckel, Scheckel.Kirk@epa.gov1, Steven Acree, acree.steven@epa.gov2, Randall Ross, ross.randall@epa.gov2, Bob Lien, lien.bob@epa.gov1, Patrick Clark, clark.patrick@epa.gov1, and Brad Scroggins, scroggins.brad@epa.gov2. (1) Land Remediation and Pollution Control Division, U.S. Environmental Protection Agency, 26 W Martin Luther King Dr, Cincinnati, OH 45268, (2) Ground Water and Ecosystems Restoration Division, U.S. Environmental Protection Agency, 919 Kerr Research Dr, Ada, OK 74820
A field investigation was conducted to examine the distribution of arsenic in ground water, surface water, and sediments at a Superfund Site in the northeastern United States (see companion presentation by K. G. Scheckel et al). Ground-water discharge into the study area was characterized as having high ferrous iron and arsenic concentrations. Patterns in ground-water discharge were assessed via a network of vertically-nested wells, piezometers, and seepage meter deployments to map out small scale variations in discharge into the surface water body. These ground-water measurements were supplemented with vertical profiling of surface water chemistry and evaluation of arsenic sequestration during iron oxide precipitation at the sediment-water interface. The mineralogy of iron oxide precipitates was determined along with in-situ arsenic sorption characteristics. This information will be employed to inform decisions on the design of appropriate remedies to address the cleanup of ground water and sediments at the site.