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Chlorine isotope investigation of natural attenuation of trichloroethene in an aerobic aquifer

Journal Article · · Environmental Science and Technology
DOI:https://doi.org/10.1021/es9802605· OSTI ID:290194
; ; ; ;  [1];  [2]
  1. Argonne National Lab., IL (United States)
  2. Lockheed-Martin Energy Services, Inc., Kevil, KY (United States)

Natural attenuation of chlorinated aliphatic hydrocarbons (CAHs) can be an important mechanism for groundwater remediation. It is difficult to determine the effectiveness of natural CAH attenuation from chemical analyses of groundwater samples because mixing, dispersion, and secondary reactions can mask the chemical evidence of attenuation. In this paper, the authors explore the application of stable chlorine isotope ratio measurements as a new tool for evaluating natural attenuation of CAHs. They report stable isotope ratios of chlorine in both trichloroethene (TCE) and inorganic chloride in groundwater from an aerobic aquifer beneath an extensively contaminated industrial site, the Paducah Gaseous Diffusion Plant in western Kentucky. Variations in the concentrations and chlorine isotope ratios of TCE and chloride in the groundwater are consistent with those expected from natural attenuation. These data support a model in which partial TCE degradation occurred in relatively impermeable, clay-rich sediments above the aquifer, and little or no further degradation of TCE occurred within the aquifer. A record of changing conditions within the TCE source area can be inferred from the spatial variation of chlorine isotope ratios for TCE and chloride within the plume.

Research Organization:
Argonne National Laboratory (ANL), Argonne, IL
Sponsoring Organization:
USDOE, Washington, DC (United States)
DOE Contract Number:
W-31109-ENG-38; AC05-76OR00001
OSTI ID:
290194
Journal Information:
Environmental Science and Technology, Journal Name: Environmental Science and Technology Journal Issue: 20 Vol. 32; ISSN 0013-936X; ISSN ESTHAG
Country of Publication:
United States
Language:
English