Cr. Chinake et al., Oxyhalogen-sulfur chemistry: Kinetics and mechanism of the oxidation of a Bunte salt 2-aminoethanethiolsulfuric acid by chlorite, PHYS CHEM P, 3(22), 2001, pp. 4957-4964
Spectrophotometric and H-1 NMR methods have been used to study the kinetics
and mechanism of oxidation of the Bunte salt, 2-aminoethanethiol sulfuric
acid, (AETSA) by chlorite in mildly acidic H2NCH2CH2S-SO3H media. The react
ion is characterized by a long quiescent induction period followed by rapid
and autocatalytic production of chlorine dioxide. The formation of chlorin
e dioxide is much more pronounced in stoichiometric excess of chlorite. The
stoichiometry of the reaction in excess chlorite just before formation of
chlorine dioxide was determined to be: 2ClO(2)(-) + H2NCH2CH2S-SO3H --> ClN
HCH2CH2SO3H + SO4-2 + Cl- + H+, while in excess AETSA the stoichiometry was
: 3ClO(2)(-) + 2H(2)NCH(2)CH(2)S-SO3H + 2H(2)O --> 2NH(2)CH(2)CH(2)SO(3)H 2SO(4)(-2) + 3Cl(-) + 4H(+). Although the products in excess chlorite also
included pure taurine and dichlorotaurine, monochlorotaurine was the domin
ant species at pH 1-3. This Bunte salt showed a facile SES bond cleavage af
ter a single S-oxygenation step on the inner sulfur atom. The sulfoxide is
quite stable but there was no experimental evidence for the existence of th
e sulfone-sulfonic acid. Sulfate production was almost quantitative for the
oxidation of only one of the sulfur atoms. Further reaction of the taurine
occurred only on the nitrogen atom with no cleavage of the CES bond. A 21-
reaction kinetics scheme model gave reasonable agreement with experiment.