HR: 11:30h
AN: H22A-05    [Abstracts]
TI: Investigation of Processes Controlling Elution of Solutes from Nonaqueous Phase Liquid (NAPL) Pools into Groundwater
AU: * Seyedabbasi, M
EM: ahmad@udel.edu
AF: Department of Civil and Environmental Engineering, 301 DuPont Hall, University of Delaware, Newark, DE 19716-3120 United States
AU: Pirestani, K
EM: katayoun.pirestani@state.de.us
AF: Department of Natural Resources and Environmental Control, 89 Kings Hwy, Dover, DE 19901 United States
AU: Holland, S B
EM: sbh@udel.edu
AF: Department of Civil and Environmental Engineering, 301 DuPont Hall, University of Delaware, Newark, DE 19716-3120 United States
AU: Imhoff, P T
EM: imhoff@ce.udel.edu
AF: Department of Civil and Environmental Engineering, 301 DuPont Hall, University of Delaware, Newark, DE 19716-3120 United States
AB: Two major processes influencing the elution of solutes from porous media contaminated with nonaqueous phase liquids (NAPLs) are external mass transfer between the NAPL and groundwater and internal diffusion through NAPL ganglia and pools. There is a relatively large body of literature on the dissolution of single-species NAPLs. Less is known about the rates of elution of compounds dissolving from multicomponent NAPLs. We examined the mass transfer of one solute, 2,3-dimethyl-2-butanol (DMB) - a partitioning tracer, between groundwater and a dense NAPL - trichloroethylene (TCE). Diffusion cell experiments were used to measure the molecular diffusion coefficient of DMB in pure TCE and in porous media contaminated with a TCE pool. Measured diffusion coefficients were compared with empirical correlations (pure TCE) and a parallel resistance model (TCE pool). Based on the results from these analyses, a dimensionless Biot number was derived to express the ratio of the external rate of mass transfer from a NAPL pool to the internal rate of diffusion within the pool, which varies with NAPL saturation and NAPL-water partition coefficient. Biot numbers were then estimated for several laboratory scale experiments involving DMB transport between NAPL pools and groundwater. The estimated Biot numbers were in good agreement with experimental results. The expression for the Biot number developed here may be used to assess the processes controlling the elution of solutes from NAPL pools, which has implications on long-term predictions of solute dissolution from NAPLs in the field.
DE: 1829 Groundwater hydrology
SC: Hydrology [H]
MN: Fall Meeting 2005