A laser flash photo lysis-resonance fluorescence kinetic study: Reaction of O(3P) with O3

The laser flash photolysis of ozone at ≈ 6000 Å has been used to generate a clean kinetic source of ground state atomic oxygen, O(³P). The decay of O(³P) due to reaction with O₃ was monitored via resonance fluorescence at 1300 Å, under static reaction cell conditions. Over the temperature range of 220–353°K, the bimolecular rate constant, k₁, could be expressed in Arrhenius form as: k₁ = (2.02 ± 0.19) × 10^?11 exp-(4522 ± 210 kcal/mole)/RT]. Units are in cm³molec^?1 sec^-1. A comparison of the results from this work with other recent investigations, indicates that the reliability of k₁ is now probably as good as 10–15% over nearly 300 degrees.