The application of ozone along with hydrogen peroxide,
commonly
referred to as peroxone oxidation, is a widely investigated technique
for wastewater treatment. Degradation of ozone in water is a key step
in the pollutant degradation mechanism, particularly in peroxone oxidation.
However, the degradation of ozone in water is not understood at a
low pH (<6). This study reveals that current ozone degradation
models overestimate degradation at a low pH because the rate constants
involved in the dissociation equilibrium of the hydroperoxyl radical
are inaccurate. Here, the rate constants of forward and backward reactions
were calculated with ab initio quantum chemical calculations
computed from the CCSD (T) theory to be 1.45 × 103 s–1 and 8.6 × 107 m3 kmol –1 s–1, respectively. After
modifying the current kinetic model by using the calculated rate constants,
the predictions of ozone half-lives at a low pH (<6) are improved
by 1–2 orders of magnitude in pure water (without organic matter
and carbonate species) in comparison with the available experimental
results. The ozone decomposition kinetic model was used to develop
a comprehensive kinetic model for peroxone oxidation of toluene. The
results demonstrate that the new rate constants considerably improve
the peroxone oxidation process as well.