Polarographic reduction of aqueous sulfur dioxide
Direct- and alternating-current polarograms of aqueous SO 2 · OH 2 solutions show four reduction waves, more than previously reported. Waves I and II probably result from the electroreduction of SO 2 · OH 2 and HSO − 3, respectively; these two waves completely overlap at pH 1 but are partially resol...
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Published in | Polyhedron Vol. 5; no. 9; pp. 1467 - 1473 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
Oxford
Elsevier Ltd
1986
New York, NY Elsevier Science |
Subjects | |
Online Access | Get full text |
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Summary: | Direct- and alternating-current polarograms of aqueous SO
2 · OH
2 solutions show four reduction waves, more than previously reported. Waves I and II probably result from the electroreduction of SO
2 · OH
2 and HSO
−
3, respectively; these two waves completely overlap at pH 1 but are partially resolved at higher pH values due to different pH dependence. Reduction of SO
2 · OH
2 involves two electrons and two H
+ ions and the initial product is probably sulfoxylic acid, H
2SO
2. This product can disproportionate to S
0 and SO
2 · OH
2 in very acidic media (pH ≤ 1) and, in the limit, double the reduction current of SO
2 · OH
2. Reduction of HSO
−
3 appears to occur via two paths: one is a two-electron three-H
+ ion path and the other is a one-electron one-H
+ ion path. The former dominates at pH ≤ 3 and probably produces H
2SO
2; the latter dominates at pH > 4 and may produce SO
−
2. H
2SO
2 in less acidic media can react with HSO
−
3 to yield dithionite species (such as H
2S
2O
4, HS
2O
−
4 and S
2O
2−
4) and HSO
2 and SO
−
2 by dissociation of the dithionite species. Waves III and IV are believed to result from reduction of HSO
2 and SO
−
2, respectively, to H
2SO
2 species. |
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ISSN: | 0277-5387 |
DOI: | 10.1016/S0277-5387(00)83508-1 |