The kinetics of the decomposition of ozone have been studied in acidic aque
ous solutions by means of spectrophotometric techniques in order to obtain
more information on the mechanism of this process. The effects of the purit
y of the oxygen gas used for preparing the ozone solution, the ozone concen
tration, ageing of the solution, pH (2-6), and the dependence on the ionic
strength of the solution were investigated. It was found that the maximum o
zone concentration and the self-decomposition of ozone in solution strongly
depend on all these factors. The individual decomposition curves could be
simulated successfully by using a simplified reaction scheme that involves
the formation of a radical chain reaction initiated by the reaction of ozon
e with hydroxide ion. This reaction scheme gives a very good representation
of the experimental data over a wide pH range (1-6) and initial ozone conc
entration (1.5-3.5 x 10(4) mol dm(3)) over a relatively long period of time
(minutes and longer). From these simulations it was possible to obtain est
imates of the equilibrium concentrations of transient species and by-produc
ts formed during the decomposition of ozone. It followed from these calcula
tions that the hydroxyl radical is the most abundant radical species and hy
drogen peroxide a major product in equilibrated ozone solutions.