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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorRIVA, Matthieu
hal.structure.identifierUniversity College Cork [UCC]
dc.contributor.authorHEALY, Robert
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorFLAUD, Pierre Marie
ORCID: 0000-0002-2331-5641
IDREF: 102543291
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorPERRAUDIN, Emilie
hal.structure.identifierUniversity College Cork [UCC]
dc.contributor.authorWENGER, John
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorVILLENAVE, Eric
dc.date.accessioned2024-09-30T09:58:23Z
dc.date.available2024-09-30T09:58:23Z
dc.date.issued2017-02
dc.identifier.issn1352-2310en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/202025
dc.description.abstractEnThis work is focused on the gas-phase oxidation of acenaphthylene and acenaphthene by OH radicals and associated secondary organic aerosol (SOA) formation under low and high-NOx conditions. Experiments were carried out in an atmospheric simulation chamber using a proton transfer reaction time-of-flight-mass spectrometer (PTR-TOF-MS) and an aerosol time-of-flight-mass spectrometer (ATOFMS) to chemically characterize the gas- and particle-phase products, respectively. Due to the structures of these two aromatic compounds, the proposed chemical mechanisms exhibit some differences. In the case of acenaphthene, H-atom abstraction from the saturated cyclopenta-fused ring was found to be competitive with the OH-addition to the aromatic rings. During the photooxidation of acenaphthene using nitrous acid (HONO), aromatic ring-opening products such as indanone and indanone carbaldehyde, generated through OH addition to the aromatic ring, were formed in higher yields compared to low-NOx conditions. In the case of acenaphthylene, OH addition to the unsaturated cyclopenta-fused ring was strongly favored. Hence, ring-retaining species such as acenaphthenone and acenaphthenequinone, were identified as the main reaction products in both gas- and particle-phases, especially under high-NOx conditions. Subsequent SOA formation was observed in all experiments and SOA yields were determined under low/high-NOx conditions to be 0.61/0.46 and 0.68/0.55 from the OH-initiated oxidation of acenaphthylene and acenaphthene, respectively.
dc.language.isoENen_US
dc.subject.enGEOF
dc.subject.enPAHs
dc.subject.enGas-phase
dc.subject.enAtmospheric oxidation
dc.subject.enPhotooxidation
dc.subject.enOH radicals
dc.title.enGas- and particle-phase products from the photooxidation of acenaphthene and acenaphthylene by OH radicals
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.atmosenv.2016.11.063en_US
dc.subject.halChimieen_US
bordeaux.journalAtmospheric Environmenten_US
bordeaux.page34-44en_US
bordeaux.volume151en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamLPTCen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-03272589
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Atmospheric%20Environment&rft.date=2017-02&rft.volume=151&rft.spage=34-44&rft.epage=34-44&rft.eissn=1352-2310&rft.issn=1352-2310&rft.au=RIVA,%20Matthieu&HEALY,%20Robert&FLAUD,%20Pierre%20Marie&PERRAUDIN,%20Emilie&WENGER,%20John&rft.genre=article


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