STABLE CHLORINE AND CARBON-ISOTOPE MEASUREMENTS OF SELECTED CHLORINATED ORGANIC-SOLVENTS

Citation
Em. Vanwarmerdam et al., STABLE CHLORINE AND CARBON-ISOTOPE MEASUREMENTS OF SELECTED CHLORINATED ORGANIC-SOLVENTS, Applied geochemistry, 10(5), 1995, pp. 547-552
Citations number
24
Categorie Soggetti
Geochemitry & Geophysics
Journal title
ISSN journal
08832927
Volume
10
Issue
5
Year of publication
1995
Pages
547 - 552
Database
ISI
SICI code
0883-2927(1995)10:5<547:SCACMO>2.0.ZU;2-4
Abstract
Stable Cl and C isotope ratio results for 3 selected chlorinated solve nts, perchloroethylene (PCE), trichloroethylene (TCE) and 1,1,1-trichl oroethane (TCA) provided by 4 different manufacturers are presented. T he isotope ratio for all compounds range between -3.5 and + 6.0 parts per thousand for delta(37)Cl and from -37.2 to -23.3 parts per thousan d for delta(13)C. The greatest Cl-37 difference between manufacturers is observed in the TCE samples which show delta(37)Cl values of -2.5 p arts per thousand for PPG, + 2.4 parts per thousand for ICI and + 4.4 parts per thousand for DOW. TCAs show a smaller range (-2.4 to +2.0 pa rts per thousand), while the TCEs have slightly different Cl-37 conten ts. The C-13 data show the most distinct delta(13)C values for PCEs (- 23.3 for DOW, -24.1 for Vulcan, - 33.8 for PPG and - 37.2 parts per th ousand for ICI) while both TCEs and TCAs show a smaller delta(13)C ran ge, but still distinct differences. These preliminary data suggest tha t each manufacturer and solvent type may have distinctive delta(37)Cl and delta(13)C values. These results show that by using a combination of Cl-37 and C-13, there is a potential to indicate a specific source of chlorinated solvents, as well as an ability to delineate contaminat ion episodes caused by these compounds in groundwaters.