Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
9530501 | Geochimica et Cosmochimica Acta | 2005 | 8 Pages |
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 10â8 M and 10â6 M, respectively.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Ann-Kathrin Leuz, C. Annette Johnson,