Abstract

Degradation of chlorinated ethenes (CEs) in low conductivity layers of aquifers reduces pollution plume tailing and accelerates natural attenuation timeframes. The degradation pathways involved are often different from those in the higher conductive layers and might go undetected when only highly conductive layers are targeted in site assessments. Reactive transport model simulations (PHT3D in FloPy) were executed to assess the performance of dual carbon and chlorine compound specific stable isotope analysis (CSIA) in degradation pathway identification and quantification in a coupled physical-chemical heterogeneous virtual aquifer. Degradation rate constants were assumed correlated to the hydraulic conductivity: positively for oxidative transformation (higher oxygen availability in coarser sands) and negatively for chemical reduction (higher content of reducing solids in finer sediments). Predicted carbon isotope ratios were highly heterogeneous. They generally increased downgradient of the pollution source but the large variation across depth illustrates that monotonously increasing isotope ratios downgradient, as were associated with the oxidative component, are not necessarily a common situation when degradation is favorable in low conductivity layers. Dual carbon-chlorine CSIA performed well in assessing the occurrence of the spatially separated degradation pathways and the overall degradation, provided appropriate enrichment factors were known and sufficiently different. However, pumping to obtain groundwater samples especially from longer well screens causes a bias towards overestimation of the contribution of oxidative transformation associated with the higher conductive zones. As degradation was less intense in these highly conductive zones under the simulated conditions, overall degradation was underestimated. In contrast, in the usual case of limited CSIA data, dual CSIA plots may rather indicate dominance of chemical reduction, while oxidative transformation could go unnoticed, despite being an equally important degradation pathway.

Highlights

  • The potential degradation of chlorinated ethenes (CEs) through both biotic and abiotic redox-sensitive pathways in groundwater (Vogel et al, 1987) opened opportunities for monitored natural attenuation (MNA) as an alternative to invasive, energy-intensive technologies for the remediation of polluted sites

  • Applying a simple correlation between the hydraulic conductivity and the two degradation rate constants of TCE, alike the approach of (Cunningham and Fadel, 2007), we investigate the resulting spatially heterogeneous carbon and chlorine isotope ratio patterns of TCE and the implications for polluted site investigation

  • This simulation study illustrates that reductive degradation of CEs in low-permeability zones might be detected using dual carbon (C) and chlorine (Cl) compound specific stable isotope analysis (CSIA), when TCE oxidation occurs in highly conductive zones

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Summary

Introduction

The potential degradation of chlorinated ethenes (CEs) through both biotic and abiotic redox-sensitive pathways in groundwater (Vogel et al, 1987) opened opportunities for monitored natural attenuation (MNA) as an alternative to invasive, energy-intensive technologies for the remediation of polluted sites. Recent studies suspect that chloroethene degradation in the presence of iron(II) minerals might have been underestimated at field sites, including at sites where degradation occurs through simultaneous abiotic and biotic degradation (Brown et al, 2007). One of the reasons would be the general lack of detection of degradation products, either due to being indiscernible from the background concentrations or because they are not measured (He et al, 2009). When trichloroethylene (TCE) is in contact with the iron hydroxides green rust or magnetite, the daughter products acetylene, ethene, and ethane are likely to degrade further in aquifers (Berns et al, 2019; Han et al, 2012; Jeong and Kim, 2007; Lee and Batchelor, 2002; Liang et al, 2009). The aerobic cometabolism of TCE, which produces CO2 and Cl, could have been overlooked

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