Article ID Journal Published Year Pages File Type
9530501 Geochimica et Cosmochimica Acta 2005 8 Pages PDF
Abstract
It could be concluded that O2 was unlikely to be a significant oxidant in homogenous solution, but that H2O2 might be responsible for the oxidation of Sb(III) in natural waters since half-lives could vary from 32 yr to 117 days at pH 8 with H2O2 concentrations between 10−8 M and 10−6 M, respectively.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
Authors
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