A mechanism
(a set of significant reactions with rate constants)
has been proposed for the complex chemical reaction of ozone with
chloride ion in aqueous solution at pH 5.5–12, leading to the
formation of chlorate ion ClO3
– as the
main product and perchlorate ion ClO4
– as a byproduct. A mathematical model of chemical reaction kinetics
in the O3–Cl–(aq) system has been
constructed. The most important chlorate formation channels are initiated
by the oxidation of chloride ion with an ozone molecule or hydroxyl
free radical. The reaction of Cl– with O3 leads to the formation of hypochlorite ion in the primary stage.
Subsequent oxidation reactions of ClO– give chlorine
dioxide ClO2
• as an intermediate. When chloride is oxidized with OH• radicals, Cl2
•– anion radicals
are formed, which then react with ozone to form chlorine monoxide
ClO•. Subsequent oxidation and combination reactions
of ClO• and ClO2
• and the hydrolysis of complex chlorine
oxides Cl2O
x
lead to the generation
of chlorate and also perchlorate. The results obtained quantitatively
characterize for the first time the complex reaction of O3 with Cl–(aq), based on the mechanism, and make
it possible to predict the kinetics of its product formation under
various conditions.