Abstract
The pH dependence of the evolution of O2 in the Fenton reaction has been studied by using an indirect method for measuring [O2]. The results confirmed observations of previous workers, namely, that the evolution of O2 diminished as the pH was lowered. A quantitative analysis of the dependence of [O2] and [Fe2+] during the reaction as a function of time showed that the pH dependence of the course of the reaction can be accounted for by assuming an acid base reaction of the active intermediate: FeO2+ + H+ ⇄ = FeOH3+ FeOH3+ is the active entity in the reaction with Fe2+ to produce Fe3+ ions, while the other form FeO2+ is involved in reactions leading to O2 evolution.
Original language | English |
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Pages (from-to) | 1734-1741 |
Number of pages | 8 |
Journal | Journal of Physical Chemistry A |
Volume | 107 |
Issue number | 11 |
DOIs | |
State | Published - 20 Mar 2003 |