Atmospheric studies of the kinetic rate law of the oxidation of dissol
ved sulphur dioxide by hydrogen peroxide are generally carried out by
laboratory measurements using reactant concentrations 10(2)-10(4) time
s higher than those in tropospheric water (clouds, fog and rain). The
present amperometric technique, based on detection of H2O2 With a rota
ting platinum anode (measurement of the oxidation current at 0.4 V/SCE
), allows us to study the kinetics at low reactant concentrations. The
results (in NaClO4 medium, at 25 degrees C) are consistent with our p
revious study. On the basis of the derived rate law, v = k(H2O2) [H+]
[HSO3-] [H2O2] and the influence of ionic strength on the third-order
rate constant (k(H2O2)), we propose a mechanism with a fast pre-equili
brium step in which some of the reactants are ionic. This is followed
by specific acid catalysis (rate-determining step). The variation of k
(H2O2) was determined as a function of ionic strength (0 less than or
equal to I less than or equal to 3 mol L(-1)).