Ozone decomposition in aqueous solution was studied by the stopped flow met
hod over the pH 10.4 - 13.2 range at 25 +/- 0.1 degrees C and I = 0.5 M NaC
lO4. At 260 nm the molar absorptivity of aqueous ozone was determined to be
3135 +/- 22 M(-1)cm(-1). It was shown that various experimental factors ma
y significantly alter the course of the reaction. Even small amounts of H2O
2 absorbed by the plastic parts of the stopped-flow instrument can affect t
he kinetic features of the reaction for an extended period of time. Under s
trictly controlled experimental conditions sufficiently reproducible data c
ould be obtained for the decomposition. The data were evaluated by comparin
g experimental and simulated kinetic traces. A detailed kinetic model was d
eveloped which is able to predict the decay and life-time of ozone as well
as the formation and decomposition of the ozonide ion radical (O-3(-)) over
the pH 10.4 - 13.2 range.