Abstract

Oxidation of Cr(III) to toxic Cr(VI) by Mn(IV) or MN(III) species has been identified as probably the only important oxidation pathway in soils, aquatic bodies, and atmospheric environments. The authors observed ready oxidation of Cr(III) in Fe(III) solutions in light at pH 3.2--4.4. Further kinetic study of this oxidation was performed in sunlight as well as in black light under controlled conditions. Quantum yields of Cr(VI) formation at 356 nm were 0.020--0.046 for initial levels of 50--800 {micro}M Cr(III) and 200 {micro}M Fe(III). The Cr(VI) formation reached steady state in 0.5 h. The best linearity found only for log[Cr(III)] vs t in the first 1 or 1.5 min of the reaction suggests apparent first-order kinetics for the disappearance of Cr(III) at 356 nm over the period; afterward, it failed to comply with any regular rate law. The Cr(III) oxidation decreased at high initial levels of Cr(III) or Fe(III) and upon removal of O{sub 2}, and it was found to be very limited at pH 5.0. Cr(III) was hypothesized to be oxidized to Cr(VI) by {sup {sm_bullet}}OH radicals from photolysis of FeOH{sup 2+} complexes; Cr(VI) also was reduced by the formed Fe(II) and intermediates such as HO{sub 2}.more » This study suggests that light-induced oxidation of aqueous Cr(III) in the presence of Fe(III) would be one potential pathway for the oxidation of Cr(III) to toxic Cr(VI), more possibly in atmospheric waters or in acidic surface waters with low dissolved organic carbon content; it would not be expected to occur in surface soils because of their universal association with organic carbon.« less

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