posted on 2016-03-09, 00:00authored byDi He, Jinxing Ma, Richard N. Collins, T. David Waite
While
it has been recognized for some time that addition of nanoparticlate
zerovalent iron (nZVI) to oxygen-containing water results in both
corrosion of Fe0 and oxidation of contaminants, there is
limited understanding of either the relationship between transformation
of nZVI and oxidant formation or the factors controlling the lifetime
and extent of oxidant production.
Using Fe K-edge extended X-ray absorption fine structure
(EXAFS) spectroscopy, we show that while nZVI particles are transformed
to ferrihydrite then lepidocrocite in less than 2 h, oxidant generation
continues for up to 10 h. The major products (Fe(II) and H2O2) of the reaction of nZVI with oxygenated water are
associated, for the most part, with the surface of particles present
with these surface-associated Fenton reagents inducing oxidation of
a target compound (in this study, 14C-labeled formate).
Effective oxidation of formate only occurred after formation of iron
oxides on the nZVI surface with the initial formation of high surface
area ferrihydrite facilitating rapid and extensive adsorption of formate
with colocation of this target compound and surface-associated Fe(II)
and H2O2 apparently critical to formate oxidation.
Ongoing formate oxidation long after nZVI is consumed combined with
the relatively slow consumption of Fe(II) and H2O2 suggest that these reactants are regenerated during the nZVI-initiated
heterogeneous Fenton process.