Stable chlorine and carbon isotope measurements of selected chlorinated organic solvents

Abstract Stable Cl and C isotope ratio results for 3 selected chlorinated solvents, perchloroethylene (PCE), trichloroethylene (TCE) and 1,1,1-trichloroethane (TCA) provided by 4 different manufacturers are presented. The isotope ratio for all compounds range between −3.5 and +6.0‰ for δ 37 Cl and from −37.2 to −23.3%. for δ 13 C . The greatest 37 Cl difference between manufacturers is observed in the TCE samples which show δ 37 CI values of −2.5%o for PPG, +2.43‰ for ICI and +4.4‰ for DOW. TCAs show a smaller range (−2.4 to +2.0‰), while the TCEs have slightly different 37 Cl contents. The 13 C data show the most distinct δ 13 C values for PCEs (−23.3 for DOW, −24.1 for Vulcan, −33.8 for PPG and −37.2‰ for ICI) while both TCEs and TCAs show a smaller δ 13 C range, but still distinct differences. These preliminary data suggest that each manufacturer and solvent type may have distinctive δ 637 Cl and δ 13 C values. These results show that by using a combination of 37 Cl and 13 C, there is a potential to indicate a specific source of chlorinated solvents, as well as an ability to delineate contamination episodes caused by these compounds in groundwaters.

[1]  J. Bracken,et al.  Theoretical effect of diffusion on isotopic abundance ratios in rocks and associated fluids , 1955 .

[2]  A. Long,et al.  Natural chlorine isotope variations , 1984, Nature.

[3]  A. Long,et al.  Production and transport of carbon dioxide in a contaminated vadose zone: a stable and radioactive carbon isotope study , 1990 .

[4]  Rosalie M. Bartholomew,et al.  CHLORINE ISOTOPE EFFECT IN REACTIONS OF TERT-BUTYL CHLORIDE , 1954 .

[5]  C. Eastoe,et al.  Stable chlorine isotopes in hydrothermal processes , 1992 .

[6]  John A. Cherry,et al.  Groundwater contamination: pump-and-treat remediation , 1989 .

[7]  P. Deines,et al.  Chapter 9 – THE ISOTOPIC COMPOSITION OF REDUCED ORGANIC CARBON , 1980 .

[8]  H. Eggenkamp δ37Cl : the geochemistry of chlorine isotopes , 1994 .

[9]  J. Cherry,et al.  37Cl-35Cl variations in a diffusion-controlled groundwater system , 1986 .

[10]  P. Klein,et al.  Comparison of quartz and Pyrex tubes for combustion of organic samples for stable carbon isotope analysis , 1983 .

[11]  A. Long,et al.  High-precision measurement of chlorine stable isotope ratios , 1993 .

[12]  S. Macko,et al.  Evidence for bacterially generated hydrocarbon gas in Canadian shield and Fennoscandian shield rocks , 1993 .

[13]  W. L. Faith,et al.  Faith, Keyes, and Clark's Industrial chemicals , 1975 .

[14]  N. Tanaka,et al.  Chlorine in the stratosphere , 1991, Nature.

[15]  R. Hinchee,et al.  Monitoring in situ biodegradation of hydrocarbons by using stable carbon isotopes , 1991 .

[16]  J. Barker,et al.  The Geochemistry and Origin of Natural Gases in Southern Ontario , 1984 .

[17]  A. J. Downs,et al.  The chemistry of chlorine, Bromine, iodine and astatine , 1975 .

[18]  R. Aravena,et al.  Dissolved organic carbon and methane in a regional confined aquifer, southern Ontario, Canada: Carbon isotope evidence for associated subsurface sources , 1993 .