Dense, viscous brine behavior in heterogeneous porous medium systems

• Published in: Journal of contaminant hydrology 2010-06, Vol.115 (1), p.46-63
• Main Authors: Wright, D. Johnson, Pedit, J.A., Gasda, S.E., Farthing, M.W., Murphy, L.L., Knight, S.R., Brubaker, G.R., Miller, C.T.
• Format: Article
• Language: English
• Subjects: Bromides; Bromides - chemistry; Calcium; Calcium Compounds - chemistry; Complex systems; Density; DNAPL; Earth sciences; Earth, ocean, space; Economics; Environmental Restoration and Remediation - economics; Environmental Restoration and Remediation - methods; Exact sciences and technology; Fingering; Hydrogeology; Hydrology; Hydrology. Hydrogeology; Instabilities; Mathematical models; Modeling; Models, Theoretical; Porosity; Remediation; Salt water; Salts - chemistry; Soil Pollutants - analysis; Solutions - chemistry; Specific Gravity; Viscosity; Water Pollutants, Chemical - analysis; Water Supply - analysis
• ISSN: 0169-7722; 1873-6009
• DOI: 10.1016/j.jconhyd.2010.03.005

The behavior of dense, viscous calcium bromide brine solutions used to remediate systems contaminated with dense nonaqueous phase liquids (DNAPLs) is considered in laboratory and field porous medium systems. The density and viscosity of brine solutions are experimentally investigated and functional forms fit over a wide range of mass fractions. A density of 1.7 times, and a corresponding viscosity of 6.3 times, that of water is obtained at a calcium bromide mass fraction of 0.53. A three-dimensional laboratory cell is used to investigate the establishment, persistence, and rate of removal of a stratified dense brine layer in a controlled system. Results from a field-scale experiment performed at the Dover National Test Site are used to investigate the ability to establish and maintain a dense brine layer as a component of a DNAPL recovery strategy, and to recover the brine at sufficiently high mass fractions to support the economical reuse of the brine. The results of both laboratory and field experiments show that a dense brine layer can be established, maintained, and recovered to a significant extent. Regions of unstable density profiles are shown to develop and persist in the field-scale experiment, which we attribute to regions of low hydraulic conductivity. The saturated–unsaturated, variable-density groundwater flow simulation code SUTRA is modified to describe the system of interest, and used to compare simulations to experimental observations and to investigate certain unobserved aspects of these complex systems. The model results show that the standard model formulation is not appropriate for capturing the behavior of sharp density gradients observed during the dense brine experiments.