H. Elias et al., KINETICS AND MECHANISM OF THE OXIDATION OF SULFUR(IV) BY PEROXOMONOSULFURIC ACID ANION, Atmospheric environment, 28(3), 1994, pp. 439-448
Stopped-flow spectrophotometry was used to study the oxidation of S(IV
) by peroxomonosulfuric acid anion, HOOSO3- (= PMS), at 285 K in the p
H range 0-12.5 in buffered aqueous solution under pseudo-first-order c
onditions (I = 1.0 M, Na2SO4). The reaction of the HSO3- ion with PMS
is subject to general-acid catalysis, that of the SO3(2-) ion is not.
Rate constants for the general-acid catalysed oxidation of S(IV) are r
eported for various buffer acids. Rate law (equation (a)) is valid for
the pH range 0-5 at zero buffer concentration. The overall equilibriu
m constant K(exp) correlates [GRAPHICS] the various protonation steps
involved in the formation of the intermediates -O3SOOSO2- and/or -O3SO
OSO2H according to equation (b). [GRAPHICS] From K(exp) = f([H]) the e
quilibrium constant K(= 19.1+/-2.1 M-1) for the formation of the inter
mediate -O3SOOSO2- from PMS and HSO3- as well as the acid dissociation
constant K(S) of the conjugate acid -O3SOOSO2H (K(S) = (4.1+/-0.9).10
(-4) M) were obtained ([H]=proton activity; pK(S1) = pK(a)(SO2)).The f
irst-order decay of the species -O3SOOSO2H with k'(H) = 134+/-33 s-1 c
ontrols the rate of S(IV) oxidation. The pK(a) of the species H2SO5+/-
, as derived from the kinetic data, is pK(R1) almost-equal-to 0.4. In
the pH range 5-8, the rate is given by equation (c) (pK(S2) = pK(a)(HS
O3-)). [GRAPHICS] At pH >8, the rate is governed by equation (d) (pK(R
2) = pK(a)(HSO5-)). [GRAPHICS] The following rate constants were obtai
ned: k(H) = (6.2+/-0.43).10(6) M-2 s-1, k(HOH) = 3.4+/-0.96 M-2 s-1, k
(SO3) = (2.3+/-0.28).10(3) M-1 s-1, and k'(SO3) = 16+/-1.4 M-1 s-1. A
mechanistic interpretation of rate laws (a)-(d) is presented. The UV a
bsorption spectra of the species -O3SOOH and SO5(2-) are given.