作者: I. Arnold , F.J. Conies
DOI: 10.1016/0022-2860(80)85139-8
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摘要: Abstract Time-resolved atomic resonance absorption spectroscopy has been used to study the reactions of ground state oxygen atoms, O(3P), formed in photodissociation ozone at 600 nm. A critical evaluation experimental procedure is made and problems arising from mismatch line profiles are discussed. The resulting temperature dependence rate constant O—O2 recombination reaction with N2 as third collision partner significantly different that reported earlier affects atmospheric model calculations.