Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/101157
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dc.contributorDepartment of Civil and Environmental Engineeringen_US
dc.creatorZeng, Len_US
dc.creatorFan, GJen_US
dc.creatorLyu, Xen_US
dc.creatorGuo, Hen_US
dc.creatorWang, JLen_US
dc.creatorYao, Den_US
dc.date.accessioned2023-08-30T04:15:25Z-
dc.date.available2023-08-30T04:15:25Z-
dc.identifier.issn0269-7491en_US
dc.identifier.urihttp://hdl.handle.net/10397/101157-
dc.language.isoenen_US
dc.publisherPergamon Pressen_US
dc.rights© 2019 Elsevier Ltd. All rights reserved.en_US
dc.rights© 2019. This manuscript version is made available under the CC-BY-NC-ND 4.0 license https://creativecommons.org/licenses/by-nc-nd/4.0/en_US
dc.rightsThe following publication Zeng, L., Fan, G. J., Lyu, X., Guo, H., Wang, J. L., & Yao, D. (2019). Atmospheric fate of peroxyacetyl nitrate in suburban Hong Kong and its impact on local ozone pollution. Environmental pollution, 252, 1910-1919 is available at https://doi.org/10.1016/j.envpol.2019.06.004.en_US
dc.subjectFormation pathwaysen_US
dc.subjectMaster chemical mechanism (MCM)en_US
dc.subjectO3 formationen_US
dc.subjectPhotochemical smogen_US
dc.subjectPrecursorsen_US
dc.titleAtmospheric fate of peroxyacetyl nitrate in suburban Hong Kong and its impact on local ozone pollutionen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.spage1910en_US
dc.identifier.epage1919en_US
dc.identifier.volume252en_US
dc.identifier.issueBen_US
dc.identifier.doi10.1016/j.envpol.2019.06.004en_US
dcterms.abstractPeroxyacetyl nitrate (PAN) is an important reservoir of atmospheric nitrogen, modulating reactive nitrogen cycle and ozone (O3) formation. To understand the origins of PAN, a field measurement was conducted at Tung Chung site (TC) in suburban Hong Kong from October to November 2016. The average level of PAN was 0.63 ± 0.05 ppbv, with a maximum of 7.30 ppbv. Higher PAN/O3 ratio (0.043–0.058) was captured on episodes, i.e. when hourly maximum O3 exceeded 80 ppbv, than on non-episodes (0.01), since O3 production was less efficient than PAN when there was an elevation of precursors (i.e. volatile organic compounds (VOCs) and nitrogen oxide (NOx)). Model simulations revealed that oxidations of acetaldehyde (65.3 ± 2.3%), methylglyoxal (MGLY, 12.7 ± 1.2%) and other oxygenated VOCs (OVOCs) (8.0 ± 0.6%), and radical cycling (12.2 ± 0.8%) were the major production pathways of peroxyacetyl (PA) radical, while local PAN formation was controlled by both VOCs and nitrogen dioxide (NO2). Among all VOC species, carbonyls made the highest contribution (59%) to PAN formation, followed by aromatics (26%) and biogenic VOCs (BVOCs) (10%) through direct oxidation/decomposition. Besides, active VOCs (i.e. carbonyls, aromatics, BVOCs and alkenes/alkynes) could stimulate hydroxyl (OH) production, thus indirectly facilitating the PAN formation. Apart from primary emissions, carbonyls were also generated from oxidation of first-generation precursors, i.e., hydrocarbons, of which xylenes contributed the most to PAN production. Furthermore, PAN formation suppressed local O3 formation at a rate of 2.84 ppbv/ppbv, when NO2, OH and hydroperoxy (HO2) levels decreased and nitrogen monoxide (NO) value enhanced. Namely, O3 was reduced by 2.84 ppbv per ppbv PAN formation. Net O3 production rate was weakened (∼36%) due to PAN photochemistry, so as each individual production and loss pathway. The findings advanced our knowledge of atmospheric PAN and its impact on O3 production. Local O3 formation was weakened by in-situ PAN formation, mostly driven by carbonyls through their direct decomposition and facilitation on OH concentration in suburban Hong Kong.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationEnvironmental pollution, Sept 2019, v. 252, pt. B, p. 1910-1919en_US
dcterms.isPartOfEnvironmental pollutionen_US
dcterms.issued2019-09-
dc.identifier.scopus2-s2.0-85070494854-
dc.identifier.pmid31227349-
dc.identifier.eissn1873-6424en_US
dc.description.validate202308 bcchen_US
dc.description.oaAccepted Manuscripten_US
dc.identifier.FolderNumberCEE-1273-
dc.description.fundingSourceRGCen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextNational Key R&D Program of China; Ministry of Science and Technology of the People's Republic of China; Hong Kong Polytechnic University; Research Institute for Sustainable Urban Development, Hong Kong Polytechnic Universityen_US
dc.description.pubStatusPublisheden_US
dc.identifier.OPUS16536977-
dc.description.oaCategoryGreen (AAM)en_US
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