Carbon isotope fractionation during abiotic reductive dehalogenation of trichloroethene (TCE).
Dehalogenation of trichloroethene (TCE) in the aqueous phase, either on palladium catalysts with hydrogen as the reductant or on metallic iron, was associated with strong changes in delta13C. In general, the delta13C of product phases were more negative than those of the parent compound and were enriched with time and fraction of TCE remaining. For dehalogenation with iron, the delta13C of TCE and products varied from -42/1000 to +5/1000. For the palladium experiments, the final product, ethane, reached the initial delta13C of TCE at completion of the dehalogenation reaction. During dehalogenation, the carbon isotope fractionation between TCE and product phases was not constant. The variation in delta13C of TCE and products offers a new monitoring tool that operates independently of the initial concentration of pollutants for abiotic degradation processes of TCE in the subsurface, and may be useful for evaluation of remediation efficiency.
Bill
M
M
Applied Geology Group, Geological Institute, University of Tübingen, Germany.
Schüth
C
C
Barth
J A
JA
Kalin
R M
RM
D002244:Carbon / Q000737:chemistry*; D006219:Halogens / Q000737:chemistry; D007501:Iron / Q000737:chemistry; D010084:Oxidation-Reduction; D010165:Palladium / Q000737:chemistry; D012989:Soil Pollutants / Q000032:analysis; D012997:Solvents / Q000737:chemistry*; D014241:Trichloroethylene / Q000737:chemistry*; D014873:Water Pollutants / Q000032:analysis
D006219:Halogens; D012989:Soil Pollutants; D012997:Solvents; D014873:Water Pollutants; D014241:Trichloroethylene; D010165:Palladium; D002244:Carbon; D007501:Iron