Reactive
oxygen species generated during the oxygenation of different
ferrous species have been documented at groundwater field sites, but
their effect on pollutant destruction remains an open question. To
address this knowledge gap, a kinetic model was developed to probe
mechanisms of •OH production and reactivity with trichloroethene
(TCE) and competing species in the presence of reduced iron minerals
(RIM) and oxygen in batch experiments. RIM slurries were formed by
combining different amounts of Fe(II) and sulfide (with Fe(II):S ratios
from 1:1 to 50:1) or Fe(II) and sulfate with sulfate reducing bacteria
(SRB) added. Extents of TCE oxidation and •OH production were
both greater with RIM prepared under more reducing conditions (more
added Fe(II)) and then amended with O2. Kinetic rate constants
from modeling indicate that •OH production from free Fe(II)
dominates •OH production from solid Fe(II) and that TCE competes
for •OH with Fe(II) and organic matter (OM). Competition with
OM only occurs in experiments with SRB, which include cells and their
exudates. Experimental results indicate that cells and/or exudates
also provide electron equivalents to reform Fe(II) from oxidized RIM.
Our work provides new insights into mechanisms and environmental significance
of TCE oxidation by •OH produced from oxygenation of RIM. However,
further work is necessary to confirm the relative importance of reaction
pathways identified here and to probe potentially unaccounted for
mechanisms that affect abiotic TCE oxidation in natural systems.