Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/80275
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dc.contributorDepartment of Civil and Environmental Engineering-
dc.creatorGong, DC-
dc.creatorWang, H-
dc.creatorZhang, SY-
dc.creatorWang, Y-
dc.creatorLiu, SC-
dc.creatorGuo, H-
dc.creatorShao, M-
dc.creatorHe, CR-
dc.creatorChen, DH-
dc.creatorHe, LY-
dc.creatorZhou, L-
dc.creatorMorawska, L-
dc.creatorZhang, YH-
dc.creatorWang, BG-
dc.date.accessioned2019-01-30T09:14:36Z-
dc.date.available2019-01-30T09:14:36Z-
dc.identifier.issn1680-7316-
dc.identifier.urihttp://hdl.handle.net/10397/80275-
dc.language.isoenen_US
dc.publisherCopernicus GmbHen_US
dc.rights© Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License (https://creativecommons.org/licenses/by/4.0/).en_US
dc.rightsThe following publication Gong, D.C., Wang, H., Zhang, S.Y., Wang, Y., Liu, S.C., Guo, H., ... & Wang, B.G. (2018). Low-level summertime isoprene observed at a forested mountaintop site in southern China : implications for strong regional atmospheric oxidative capacity. Atmospheric chemistry and physics, 18 (19), 14417-14432 is available at https://dx.doi.org/10.5194/acp-18-14417-2018en_US
dc.titleLow-level summertime isoprene observed at a forested mountaintop site in southern China : implications for strong regional atmospheric oxidative capacityen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.spage14417-
dc.identifier.epage14432-
dc.identifier.volume18-
dc.identifier.issue19-
dc.identifier.doi10.5194/acp-18-14417-2018-
dcterms.abstractTo investigate the atmospheric oxidative capacity (AOC) in forested high mountain areas adjacent to the photochemistry-active Pearl River Delta (PRD) region in southern China, one-month online observations of isoprene and its oxidation products methyl vinyl ketone (MVK) and methacrolein (MACR) were conducted at a national background station in Nanling Mountains in summer 2016. The results showed that the observed daytime isoprene levels (377 +/- 46 pptv) were significantly lower in comparison with other forest sites within and outside China, although the sampling site was surrounded with subtropical evergreen broad-leaved trees which are strong isoprene emitters. Also, high daytime (MVK MACR)/isoprene ratios (1.9 +/- 0.5) were observed. Based on the observations, we hypothesized that the lower isoprene levels in the study forest might be attributable to a strong AOC in relation to the elevated regional complex air pollution. In further data analyses, high site-level concentrations of daytime OH (7.3 +/- 0.5 x 10(6) molecules cm(-3)) and nighttime NO3 radicals (6.0 +/- 0.5 x 10(8) molecules cm(-3)) were estimated by using a photochemical box model incorporating the master chemical mechanism (PBM-MCM), and high regional mixing ratios of OH (19.7 +/- 2.3 x 10(6) molecules cm(-3)) during 09:00-15:00 LT were also obtained by applying a parameterization method with measured aromatic hydrocarbons. And besides, high initial mixing ratios (1213 +/- 108 pptv) and short atmospheric reaction time (0.27 h) of isoprene during the day were derived by a sequential reaction approach. All these indicate that isoprene was rapidly and highly oxidized in this forest, which supports our hypothesis. The study suggests that the complex air pollution in the PRD may have significantly elevated the background AOC of the adjacent forests, and probably affects the regional air quality and ecological environment in the long term. The feedback of forest ecosystems to the increasing AOC in southern China warrants further studies.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationAtmospheric chemistry and physics, Oct. 2018, v. 18, no. 19, p. 14417-14432-
dcterms.isPartOfAtmospheric chemistry and physics-
dcterms.issued2018-
dc.identifier.isiWOS:000446731000008-
dc.identifier.scopus2-s2.0-85054798362-
dc.identifier.eissn1680-7324-
dc.description.validate201901 bcrc-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_IR/PIRAen_US
dc.description.pubStatusPublisheden_US
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