Abstract

A permeable reactive barrier, consisting of both zero valent iron (ZVI) and a biodegradable organic carbon, was evaluated for the remediation of 1,1,2-trichloroethane (1,1,2-TCA) contaminated groundwater. During an 888day laboratory column study, degradation rates initially stabilized with a degradation half-life of 4.4±0.4days. Based on the accumulation of vinyl chloride (VC) and limited production of 1,1-dichloroethene (1,1-DCE) and 1,2-dichloroethane (1,2-DCA), the dominant degradation pathway was likely abiotic dichloroelimination to form VC. Degradation of VC was not observed based on the accumulation of VC and limited ethene production.After a step reduction in the influent concentration of 1,1,2-TCA from 170±20mgL−1 to 39±11mgL−1, the degradation half-life decreased 5-fold to 0.83±0.17days. The isotopic enrichment factor of 1,1,2-TCA also changed after the step reduction from −14.6±0.7‰ to −0.72±0.12‰, suggesting a possible change in the degradation mechanism from abiotic reductive degradation to biodegradation. Microbiological data suggested a co-culture of Desulfitobacterium and Dehalococcoides was responsible for the biodegradation of 1,1,2-TCA to ethene.

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