Abstract
We report a theoretical study of the title four-atom atmospheric reaction for a wide range of initial vibrational quantum numbers (ν′, ν″). All calculations have employed the quasiclassical trajectory method, and a realistic potential energy surface obtained by using the double many-body expansion (DMBE) method. The implications of the results on a recently proposed hypothesis to explain the ‘ozone deficit’ problem are tentatively assessed.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
