The production of oxygen atoms, O(3PJ), following deactivation of photolytically generated O(2 1D2) via was monitored using time-resolved atomic absorption analysis in the vacuum ultraviolet. The measured overall rate constant for O2(b 1Σg+) deactivation by O3, 1.8±0.2×10−11 cm3 molecule−1 s−1, and total yield of ground state O(3PJ) following quenching of O2(b 1Σg+) by O3, 0.61±0.06, are in good agreement with a previous study. These results suggest that the reaction of O2(b 1Σg+) with O3 may play a role in fixing the overall density of oxygen atoms in the stratosphere.
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Amimoto et al. (1980) studied this question.
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