Classical and quasi-classical trajectory calculations of isotope exchange and ozone formation proceeding through O+O2 collision complexes

Thomas A. Baker, Gregory I. Gellene

Research output: Contribution to journalArticle

25 Scopus citations

Abstract

Ozone formation rate was determined using the calculated O3* survival time (ST) distribution. The absolute rate of ozone formation over the broad range of temperature (T=130-370K) and density (ρM-1018-1022cm-3) was modeled.

Original languageEnglish
Pages (from-to)7603-7613
Number of pages11
JournalJournal of Chemical Physics
Volume117
Issue number16
DOIs
StatePublished - Oct 22 2002

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