posted on 2003-08-02, 00:00authored byJiankang Wang, James Farrell
Metallic iron filings are commonly employed as reducing
agents in permeable barriers used for remediating
groundwater contaminated by chlorinated solvents.
Reactions of trichloroethylene (TCE) and tetrachloroethylene
(PCE) with zerovalent iron were investigated to determine
the role of atomic hydrogen in their reductive dechlorination.
Experiments simultaneously measuring dechlorination and
iron corrosion rates were performed to determine the
fractions of the total current going toward dechlorination
and hydrogen evolution. Corrosion rates were determined
using Tafel analysis, and dechlorination rates were
determined from rates of byproduct generation. Electrochemical impedance spectroscopy (EIS) was used to
determine the number of reactions that controlled the
observed rates of chlorocarbon disappearance, as well
as the role of atomic hydrogen in TCE and PCE reduction.
Comparison of iron corrosion rates with those for TCE
reaction showed that TCE reduction occurred almost
exclusively via atomic hydrogen at low pH values and via
atomic hydrogen and direct electron transfer at neutral
pH values. In contrast, reduction of PCE occurred primarily
via direct electron transfer at both low and neutral pH
values. At low pH values and micromolar concentrations,
TCE reaction rates were faster than those for PCE due
to more rapid reduction of TCE by atomic hydrogen. At
neutral pH values and millimolar concentrations, PCE reaction
rates were faster than those for TCE. This shift in relative
reaction rates was attributed to a decreasing contribution
of the atomic hydrogen reaction mechanism with increasing
halocarbon concentrations and pH values. The EIS data
showed that all the rate limitations for TCE and PCE
dechlorination occurred during the transfer of the first
two electrons. Results from this study show that differences
in relative reaction rates of TCE and PCE with iron are
dependent on the significance of the reduction pathway
involving atomic hydrogen.