Assessment of 2,4-Dinitroanisole Transformation Using Compound-Specific Isotope Analysis after in Situ Chemical Reduction of Iron Oxides

Matthew J. Berens, Thomas B. Hofstetter, Jakov Bolotin, William A. Arnold

Research output: Contribution to journalArticlepeer-review

1 Scopus citations

Abstract

Ferrous iron-bearing minerals are important reductants in the contaminated subsurface, but their availability for the reduction of anthropogenic pollutants is often limited by competition with other electron acceptors including microorganisms and poor accessibility to Fe(II) in complex hydrogeologic settings. The supply of external electron donors through in situ chemical reduction (ISCR) has been proposed as one remediation approach, but the quantification of pollutant transformation is complicated by the perturbations introduced to the subsurface by ISCR. Here, we evaluate the application of compound specific isotope analysis (CSIA) for monitoring the reduction of 2,4-dinitroanisole (DNAN), a component of insensitive munitions formulations, by mineral-bound Fe(II) generated through ISCR of subsurface material from two field sites. Electron balances from laboratory experiments in batch and column reactors showed that 3.6% to 11% of the total Fe in the sediments was available for the reduction of DNAN and its partially reduced intermediates after dithionite treatment. The extent of DNAN reduction was successfully quantified from its N isotope fractionation measured in the column effluent based on the derivation of a N isotope enrichment factor, ϵN, derived from a comprehensive series of isotope fractionation experiments with numerous Fe(II)-bearing minerals as well as dithionite-reduced subsurface materials. Our observations illustrate the utility of CSIA as a robust approach to evaluate the success of in situ remediation through abiotic contaminant reduction.

Original languageEnglish (US)
Pages (from-to)5520-5531
Number of pages12
JournalEnvironmental Science and Technology
Volume54
Issue number9
DOIs
StatePublished - May 5 2020

Bibliographical note

Funding Information:
This work was supported by the Strategic Environmental Research and Development Program (SERDP, Project No. ER2618). Thanks to Lee Penn (UMN, Department of Chemistry) for allowing use of the X-ray diffractometer and to Jeanette L. Voelz (UMN, Department of Chemistry) for providing the hematite nanoparticles used in this study. ICP-OES analyses were performed by Clare Johnston (UMN, Department of Chemistry).

Publisher Copyright:
© 2020 American Chemical Society.

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