Effect of Structural Transformation of Nanoparticulate Zero-Valent Iron on Generation of Reactive Oxygen Species
Author(s) -
Di He,
Jinxing Ma,
Richard N. Collins,
T. David Waite
Publication year - 2016
Publication title -
environmental science and technology
Language(s) - English
Resource type - Journals
eISSN - 1520-5851
pISSN - 0013-936X
DOI - 10.1021/acs.est.5b04988
Subject(s) - formate , ferrihydrite , zerovalent iron , lepidocrocite , chemistry , adsorption , inorganic chemistry , extended x ray absorption fine structure , redox , oxygen , oxidation state , catalysis , goethite , absorption spectroscopy , organic chemistry , physics , quantum mechanics
While it has been recognized for some time that addition of nanoparticlate zerovalent iron (nZVI) to oxygen-containing water results in both corrosion of Fe(0) 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, (14)C-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.
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