Numerical simulations of radon as an in situ partitioning tracer for quantifying NAPL contamination using push–pull tests

• Published in: Journal of contaminant hydrology Vol. 78; no. 1; pp. 87 - 103
• Main Authors: Davis, B.M., Istok, J.D., Semprini, L.
• Format: Journal Article
• Language: English
• Published: Amsterdam Elsevier B.V 01.06.2005; Elsevier Science
• Subjects: aquifers; Computer Simulation; Earth sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; Environmental Monitoring - methods; Exact sciences and technology; Geochemistry; groundwater contamination; groundwater flow; Hydrogeology; hydrologic models; Hydrology. Hydrogeology; mathematical models; Mineralogy; NAPL; nonaqueous phase liquids; Partitioning; Pollution, environment geology; Radioactive Tracers; Radon; Radon - analysis; radon breakthrough curve; Silicates; Single-well tests; Tracers; Trichloroethylene - analysis; Water geochemistry; Water Pollutants, Chemical - analysis; NAPL; Partitioning; Radon; Tracers; Single-well tests; experimental studies; radon; models; dense nonaqueous phase liquids; bromides; nonaqueous phase liquids; tracers; ground water; concentration; digital simulation; pollution; halides; heterogeneity; in situ; contamination; saturation; remediation; aquifers; dispersion; laboratory studies
• ISSN: 0169-7722; 1873-6009
• DOI: 10.1016/j.jconhyd.2005.03.003

Presented here is a reanalysis of results previously presented by Davis et al. (2002) [Davis, B.M., Istok, J.D., Semprini, L., 2002. Push–pull partitioning tracer tests using radon-222 to quantify non-aqueous phase liquid contamination. J. Contam. Hydrol. 58, 129–146] of push–pull tests using radon as a naturally occurring partitioning tracer for evaluating NAPL contamination. In a push–pull test where radon-free water and bromide are injected, the presence of NAPL is manifested in greater dispersion of the radon breakthrough curve (BTC) relative to the bromide BTC during the extraction phase as a result of radon partitioning into the NAPL. Laboratory push–pull tests in a dense or DNAPL-contaminated physical aquifer model (PAM) indicated that the previously used modeling approach resulted in an overestimation of the DNAPL (trichloroethene) saturation ( S n). The numerical simulations presented here investigated the influence of (1) initial radon concentrations, which vary as a function of S n, and (2) heterogeneity in S n distribution within the radius of influence of the push–pull test. The simulations showed that these factors influence radon BTCs and resulting estimates of S n. A revised method of interpreting radon BTCs is presented here, which takes into account initial radon concentrations and uses non-normalized radon BTCs. This revised method produces greater radon BTC sensitivity at small values of S n and was used to re-analyze the results from the PAM push–pull tests reported by Davis et al. The re-analysis resulted in a more accurate estimate of S n (1.8%) compared with the previously estimated value (7.4%). The revised method was then applied to results from a push–pull test conducted in a light or LNAPL-contaminated aquifer at a field site, resulting in a more accurate estimate of S n (4.1%) compared with a previously estimated value (13.6%). The revised method improves upon the efficacy of the radon push–pull test to estimate NAPL saturations. A limitation of the revised method is that ‘background’ radon concentrations from a non-contaminated well in the NAPL-contaminated aquifer are needed to accurately estimate NAPL saturation. The method has potential as a means of monitoring the progress of NAPL remediation.