Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/102509
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dc.contributorDepartment of Civil and Environmental Engineeringen_US
dc.creatorLu, Hen_US
dc.creatorLyu, Xen_US
dc.creatorCheng, Hen_US
dc.creatorLing, Zen_US
dc.creatorGuo, Hen_US
dc.date.accessioned2023-10-26T07:19:02Z-
dc.date.available2023-10-26T07:19:02Z-
dc.identifier.issn2050-7887en_US
dc.identifier.urihttp://hdl.handle.net/10397/102509-
dc.language.isoenen_US
dc.publisherRoyal Society of Chemistryen_US
dc.rightsThis journal is © The Royal Society of Chemistry 2019en_US
dc.rightsThe following publication Lu, H., Lyu, X., Cheng, H., Ling, Z., & Guo, H. (2019). Overview on the spatial–temporal characteristics of the ozone formation regime in China. Environmental Science: Processes & Impacts, 21(6), 916-929 is available at https://doi.org/10.1039/C9EM00098D.en_US
dc.titleOverview on the spatial–temporal characteristics of the ozone formation regime in China,en_US
dc.typeJournal/Magazine Articleen_US
dc.description.otherinformationTitle on author’s file: "Overview on the spatial-temporal characteristics of ozone formation regime in China"en_US
dc.identifier.spage916en_US
dc.identifier.epage929en_US
dc.identifier.volume21en_US
dc.identifier.issue6en_US
dc.identifier.doi10.1039/c9em00098den_US
dcterms.abstractOzone (O3), a main component in photochemical smog, is a secondary pollutant formed through complex photochemical reactions involving nitrogen oxides (NOx) and volatile organic compounds (VOCs). In the past few decades, with the rapid economic development, industrialization and urbanization, the mixing ratio of O3 has increased substantially in China. O3 non-attainment days have been frequently observed. Despite great efforts made in the past few years, it is still difficult to alleviate O3 pollution in China, due to its non-linear relationship with the precursors. In view of the severe situation in China, this study presents a comprehensive review on the spatial–temporal variations of the relationship between O3 and its precursors (i.e. O3 formation regime), built upon the previous reviews of the spatial–temporal variations of O3 and its precursor levels. Valuable findings from previous studies are laid out for a better understanding of O3 pollution, followed by implications for the control of O3 pollution. This literature review indicates that O3 formation in most areas of the North China Plain (NCP), Yangtze River Delta (YRD) and Pearl River Delta (PRD) regions is in a VOC-limited regime during the high-O3 seasons due to dramatic emissions from human activities in cities. Outside these metropolitan areas, a NOx-limited regime dominates rural/remote areas. From summer to winter, the O3 formation regime over China shows a tendency to shift to a VOC-limited regime. Furthermore, O3 formation in China shifted toward increasing sensitivity to VOC emissions before the 12th Five-Year-Plan. However, after the 12th Five-Year-Plan, successful reduction of NOx slowed down this trend. Further effective control of VOCs is expected to achieve sustained O3 attainment in the future. To timely solve the current O3 pollution problem, precise control of O3 precursors is proposed, together with the joint prevention and control of regional air pollution.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationEnvironmental science processes & impacts, 1 June 2019, v. 21, no. 6, p. 916-929en_US
dcterms.isPartOfEnvironmental science processes & impactsen_US
dcterms.issued2019-06-01-
dc.identifier.scopus2-s2.0-85067551047-
dc.identifier.pmid31089656-
dc.identifier.eissn2050-7895en_US
dc.description.validate202310 bcchen_US
dc.description.oaAccepted Manuscripten_US
dc.identifier.FolderNumberCEE-1365-
dc.description.fundingSourceRGCen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextNational Key R&D Program of Chinaen_US
dc.description.pubStatusPublisheden_US
dc.identifier.OPUS19904418-
dc.description.oaCategoryGreen (AAM)en_US
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