Please use this identifier to cite or link to this item: https://hdl.handle.net/10316/10355
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dc.contributor.authorZhang, Lei-
dc.contributor.authorLuo, Pingya-
dc.contributor.authorHuang, Zhiyu-
dc.contributor.authorVarandas, António J. C.-
dc.date.accessioned2009-06-25T12:55:20Z-
dc.date.available2009-06-25T12:55:20Z-
dc.date.issued2006-12-28-
dc.identifier.citationThe Journal of Physical Chemistry A. 110:51 (2006) 13836-13842en_US
dc.identifier.issn1089-5639-
dc.identifier.urihttps://hdl.handle.net/10316/10355-
dc.description.abstractThe dynamics of the title five-atom atmospheric reaction is studied by the quasiclassical trajectory method for vibrational states of OH over the range 2 ≤ v ≤ 9 and initial vibrational energies of O3 between 9 and 21 kcal mol-1 using a previously reported double many-body expansion potential energy surface for HO4(2A). The results show that the reaction is controlled by both capture- and barrier-type mechanisms, with the rate constants depending strongly on the reactants' internal energy content. Also suggested from the magnitude of the calculated rate coefficients is that the title processes may not be ignorable when studying the stratospheric ozone budget.en_US
dc.language.isoengen_US
dc.publisherAmerican Chemical Societyen_US
dc.rightsopenAccesseng
dc.titleDynamics Study of the OH + O3 Atmospheric Reaction with Both Reactants Vibrationally Exciteden_US
dc.typearticleen_US
dc.identifier.doi10.1021/jp066273j-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.openairetypearticle-
item.cerifentitytypePublications-
item.grantfulltextopen-
item.fulltextCom Texto completo-
item.languageiso639-1en-
crisitem.author.researchunitCQC - Coimbra Chemistry Centre-
crisitem.author.parentresearchunitFaculty of Sciences and Technology-
crisitem.author.orcid0000-0003-1501-3317-
Appears in Collections:FCTUC Química - Artigos em Revistas Internacionais
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