EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Reactive transport of dichloromethane in laboratory aquifers: insights from dual-element isotope analysis and biomolecular approaches

Maria Prieto Espinoza1, Sylvain Weill1, Benjamin Belfort1, François Lehmann1, Jérémy Masbou1, Emilie Müller2, Stéphane Vuilleumier2, and Gwenaël Imfeld1
Maria Prieto Espinoza et al.
  • 1Laboratory of Hydrology and Geochemistry of Strasbourg, (LHyGeS UMR 7517), University of Strasbourg, CNRS, ENGEES, Strasbourg 67000, France
  • 2University of Strasbourg, CNRS, (GMGM - UMR 7156), Strasbourg 67000, France

Dichloromethane (DCM) is a toxic industrial solvent frequently detected in multi-contaminated aquifers. DCM often co-occurs with chlorinated ethenes resulting in complex mixtures posing challenges to predict its fate in groundwater. Changes in hydrochemistry and redox conditions in groundwater due to fluctuations in the water table may affect the extent and pathways of pollutant biodegradation. In this context, Compound-Specific Isotope Analysis (CSIA) is a useful tool to evaluate natural degradation of halogenated hydrocarbons. In this study, the impact of water table fluctuations on DCM biodegradation was examined in two laboratory aquifers using dual-element isotope analysis - the stable isotope fractionation of two elements (e.g., 13C and 37Cl), and high-throughput biomolecular approaches. The aquifers were supplied with contaminated groundwater from the former industrial site Thermeroil (France). High-resolution sampling and monitoring of pore water allowed examining, under steady and transient conditions, the aquifers response with respect to hydrochemistry and microbial composition. A dual C-Cl stable isotope approach (ΛC/Cl = Δδ13C/Δδ37Cl) was developed using GC-IRMS (C-DCM) and GC-MS (Cl-DCM) to estimate the extent of DCM degradation and to identify DCM degradation pathways. Under the experimental steady conditions, dissolved oxygen (<1.2 mg/L) and increasing Fe2+ concentrations at lower depths of the aquifer models indicated iron-reducing prevailing conditions, while mass transfer of oxygen increased during water table fluctuations. Pronounced carbon isotope fractionation of DCM was associated with larger DCM mass removal under transient conditions (>90%) compared to steady conditions (mass removal of 35%). Under transient conditions, carbon enrichment factors (εC) became larger over time ranging from -18.9 ± 3.4‰ to -33 ± 0.3‰ whereas chlorine enrichment factors (εCl) remained constant (-3.6 ± 0.7‰). In contrast, a similar εC of -20 ± 3.5‰ (beginning of transient condition) but a larger εCl of -10.8 ± 2‰ were determined under steady conditions. As ΛC/Cl values are independent of complicating masking effects, and thus reflect reaction mechanisms, dual C-Cl isotope plots suggested distinct DCM degradation pathways under steady and transient conditions with ΛC/Cl values of 1.68 ± 0.26 and 3.41 ± 0.50, respectively. Even though a contribution of different mechanisms may take place during transient conditions, ΛC/Cl values fall in the range of SN1 pathways reported for Ca. Dichloromethanomonas elyunquensis (ΛC/Cl = 3.40 ± 0.03).  The distinct ΛC/Cl values may imply mechanistically distinct C-Cl bond cleavage reactions subjected to microbial adaptations during dynamic hydrogeological conditions. Although bacterial communities did not significantly change over time, the occurrence of Geobacter under both steady and transient conditions supports DCM degradation under iron-reducing prevailing conditions. Altogether, our results highlight that water table fluctuations enhance DCM biodegradation and influence DCM degradation pathways compared to steady conditions. This integrative study provides new insights into in situ degradation of DCM in contaminated aquifers and accounts the effects of dynamic water tables on DCM degradation.

How to cite: Prieto Espinoza, M., Weill, S., Belfort, B., Lehmann, F., Masbou, J., Müller, E., Vuilleumier, S., and Imfeld, G.: Reactive transport of dichloromethane in laboratory aquifers: insights from dual-element isotope analysis and biomolecular approaches, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-15103,, 2020


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