Kinetics and mechanism of the oxidation of sulfur (IV) by peroxomonosulfuric acid anion
Stopped-flow spectrophotometry was used to study the oxidation of S(IV) by peroxomonosulfuric acid anion, HOOSO 3 − (=PMS), at 285 K in the pH range 0–12.5 in buffered aqueous solution under pseudo-first-order conditions ( I = 1.0 M, Na 2SO 4). The reaction of the HSO 3 − ion with PMS is subject to...
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Veröffentlicht in: | Atmospheric environment (1994) 1994, Vol.28 (3), p.439-448 |
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Zusammenfassung: | Stopped-flow spectrophotometry was used to study the oxidation of S(IV) by peroxomonosulfuric acid anion, HOOSO
3
− (=PMS), at 285 K in the pH range 0–12.5 in buffered aqueous solution under pseudo-first-order conditions (
I = 1.0 M, Na
2SO
4). The reaction of the HSO
3
− ion with PMS is subject to general-acid catalysis, that of the SO
3
2− ion is not. Rate constants for the general-acid catalysed oxidation of S(IV) are reported for various buffer acids.
Rate law (equation (a)) is valid for the pH range 0–5 at zero buffer concentration. The overall equilibrium constant
K
exp correlates
Rate=
k·K
exp
[
PMS]
0[S(IV)
]
0
1+K
exp
[
S(IV)]
0
the various protonation steps involved in the formation of the intermediates
−O
3SOOSO
2
− and/or
−O
3SOOSO
2H according to equation (b).
K
exp
=
K·(1+
[
H]
K
S1
)
(1+
[1+
H]
K
R1
)·(1+
[
H]
K
S1
)
From
K
exp
= ƒ([
H])
the equilibrium constant
K(=19.1 ±2.1 M
−1) for the formation of the intermediate
−O
3SOOSO
3
− from PMS and HSO
3
− as well as the acid dissociation constant
K
s of the conjugate acid
−O
3SOOSO
2H (
K
s=(4.1 ± 0.9) · 10
−4 M) were obtained ([H] = proton activity;
pK
s1 =
pK
a (SO
2)).
The first-order decay of the species
−O
3SOOSO
2H with
k
H
′ = 134 ± 33 s
−1 controls the rate of S(IV) oxidation. The
pK
a of the species H
2SO
5
±, as derived from the kinetic data, is
pK
R1≈0.4.
In the pH range 5–8, the rate is given by equation (c) (
pK
s2=
pK
a (HSO
3
−)).
Rate=[
k
H
[
H]+k
HOH
[H
2O
1+
K
S2
[
H]
+
k′
SO3
1+
K
S2
[
H]
]
·[
S(IV)]
0[PMS]
0
At pH>8, the rate is governed by equation (d) (
pK
R2 =
pK
a (HSO
5
−)).
Rate=
[
k
SO3
[
H]
k
R2
+k′[
SO3
1+[
H]
K
R2
]
·[
S(IV)]
0[PMS]
0
The following rate constants were obtained:
k
H = (6.2 ± 0.43)·10
6 M
−2 s
−1,
k
HOH = 3.4 ± 0.96 M
−2 s
−1,
k
SO
3
= (2.3±0.28)·10
3 M
−1 s
−1, and
k
SO
3
′ = 16 ± 1.4 M
−1 s
−1. A mechanistic interpretation of rate laws (a)–(d) is presented. The UV absorption spectra of the species
−O
3SOOH and SO
5
2− are given. |
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ISSN: | 1352-2310 1873-2844 |
DOI: | 10.1016/1352-2310(94)90122-8 |