Oxidation of Sb(III) to Sb(V) by O 2 and H 2O 2 in aqueous solutions
Abstract
The rates of Sb(III) oxidation by O 2 and H 2O 2 were determined in homogeneous aqueous solutions. Above pH 10, the oxidation reaction of Sb(III) with O 2 was first order with respect to the Sb(III) concentration and inversely proportional to the H + concentrations at a constant O 2 content of 0.22 × 10 -3 M. Pseudo-first-order rate coefficients, k obs, ranged from 3.5 × 10 -8 s -1 to 2.5 × 10 -6 s -1 at pH values between 10.9 and 12.9. The relationship between k obs and pH was: logk=1.0(±0.3)pH-18.5(±3.4)R2=0.89 No significant Sb(III) oxidation by O 2 was observed between pH 3.6 and 9.8 within 200 days. Oxidation of Sb(III) by H 2O 2 was found to be first order with respect to the total Sb(III), H 2O 2 and inversely proportional to the H + concentrations in a pH range of 8.1 to 11.7. Above pH 11.7 no pH dependence was observed. The rate law for the pH range 8.1 to 12.9 was determined to be: -{d[}/{dt}=k×[×[ and k=k3×{K1}/{K+[H+]}=k4×{K2}/{K+[H+]} where K a1 and K a2 are the deprotonation constants of Sb(OH) 3 and H 2O 2, respectively, and k 3 (=365 M -1 s -1) and k 4 (=342 M -1 s -1) are the specific second-order rate coefficients. The results indicate that the rate-limiting step below pH 11.7 involves one deprotonated species, either Sb(OH) 4- or HO 2-. Since the pK a-values of Sb(OH) 3 and H 2O 2 are very close (11.8 and 11.6, respectively), it was not possible to determine which species is involved. Varying the ionic strength between 0.001 and 1.0 M at pH 10 and between 0.01 and 1.0 M at pH 12 resulted in a less than twofold increase in k obs. In both cases, the increase was attributed to a shift in pK a-values as a function of the ionic strength. It could be concluded that O 2 was unlikely to be a significant oxidant in homogenous solution, but that H 2O 2 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 H 2O 2 concentrations between 10 -8 M and 10 -6 M, respectively.
- Publication:
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Geochimica et Cosmochimica Acta
- Pub Date:
- March 2005
- DOI:
- Bibcode:
- 2005GeCoA..69.1165L