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Evaluation of α- and β-pinene degradation in the detailed tropospheric chemistry mechanism, MCM v3.1, using environmental chamber data

dc.contributor.authorPinho, P. G.
dc.contributor.authorPio, C. A.
dc.contributor.authorCarter, W. P. L.
dc.contributor.authorJenkin, M. E.
dc.date.accessioned2017-01-27T10:28:29Z
dc.date.available2017-01-27T10:28:29Z
dc.date.issued2007
dc.description.abstractThe representation of the degradation of the monoterpenes, α- and β-pinene, in version 3.1 of the Master Chemical Mechanism (MCM v3.1) has been evaluated, using environmental chamber data from the Statewide Air Pollution Research Center (SAPRC) at the University of California. As part of this evaluation, a representation of the reactions of the monoterpenes with O(3P) has also been included, these reactions being significant under chamber conditions but generally insignificant under atmospheric conditions. The results demonstrate that MCM v3.1 provides a consistent description of the photo-oxidation of α-pinene/NOX mixtures for a range of initial VOC/NOX, but with the formation rate of ozone and decay rate of α-pinene generally being overestimated. Sensitivity of the system to parameter uncertainties and mechanistic variations proposed in the literature are described. The collective implementation of a number of refinements allows the simulations to be brought into good agreement with the experimental observations for the complete series of experiments, with each of the refinements being consistent with reported parameter uncertainty ranges or mechanistic adjustments. The system is particularly sensitive to the magnitudes of sources and sinks of free radicals. The impacts of several other reported mechanistic variations which potentially influence the first generation product distribution and the ozone formation chain length of the initial oxidation step are also described and assessed. MCM v3.1 is shown to provide a reasonable, but less consistent, description of photo-oxidation of β-pinene/NOX mixtures. The simulated magnitudes of the ozone formation rates and β-pinene removal rates are broadly comparable with the experimental observations, but the mechanism tends towards overestimation of ozone formation at low VOC/NOX and underestimation at high VOC/NOX. Implementation of a number of mechanistic variations reported in the literature does not allow the associated simulations to be brought into good agreement with the observations for the entire VOC/NOX range. The system is particularly sensitive to changes which influence the formation of HCHO (and resultant radical production upon its photolysis), and the impacts of the tested mechanistic variations are usually dominated by this effect. As a result of this work, gaps and uncertainties in the kinetic, mechanistic and chamber database for the monoterpenes are identified and discussed.pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.citationPinho, P.G., Pio, C.A., Carter, W.P.L. et al. J Atmos Chem (2007) 57: 171. doi:10.1007/s10874-007-9071-0pt_PT
dc.identifier.doi10.1007/s10874-007-9071-0pt_PT
dc.identifier.issn0167-7764
dc.identifier.urihttp://hdl.handle.net/10400.19/4111
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherSpringerpt_PT
dc.relation.publisherversionhttp://link.springer.com/article/10.1007/s10874-007-9071-0pt_PT
dc.subjectVOC oxidationpt_PT
dc.subjectα-pinenept_PT
dc.subjectβ-pinenept_PT
dc.subjectTropospheric chemistrypt_PT
dc.subjectDegradation mechanismspt_PT
dc.subjectEnvironmental chamber datapt_PT
dc.subjectOzone modellingpt_PT
dc.titleEvaluation of α- and β-pinene degradation in the detailed tropospheric chemistry mechanism, MCM v3.1, using environmental chamber datapt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.citation.endPage202pt_PT
oaire.citation.issue2pt_PT
oaire.citation.startPage171pt_PT
oaire.citation.titleJournal of Atmospheric Chemistrypt_PT
oaire.citation.volume57pt_PT
rcaap.rightsrestrictedAccesspt_PT
rcaap.typearticlept_PT

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