Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/115933
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dc.contributorDepartment of Civil and Environmental Engineering-
dc.creatorZou, Z-
dc.creatorChen, T-
dc.creatorChen, Q-
dc.creatorSun, W-
dc.creatorHan, S-
dc.creatorRen, Z-
dc.creatorLi, X-
dc.creatorSong, W-
dc.creatorGe, A-
dc.creatorWang, Q-
dc.creatorTian, X-
dc.creatorPei, C-
dc.creatorWang, X-
dc.creatorZhang, Y-
dc.creatorWang, T-
dc.date.accessioned2025-11-18T06:48:11Z-
dc.date.available2025-11-18T06:48:11Z-
dc.identifier.issn1680-7316-
dc.identifier.urihttp://hdl.handle.net/10397/115933-
dc.language.isoenen_US
dc.publisherCopernicus GmbHen_US
dc.rights©Author(s) 2025. 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 Zou, Z., Chen, T., Chen, Q., Sun, W., Han, S., Ren, Z., Li, X., Song, W., Ge, A., Wang, Q., Tian, X., Pei, C., Wang, X., Zhang, Y., and Wang, T.: Observation and modeling of atmospheric OH and HO2∗ radicals at a subtropical rural site and implications for secondary pollutants, Atmos. Chem. Phys., 25, 8147–8161 is available at https://doi.org/10.5194/acp-25-8147-2025, 2025.en_US
dc.titleObservation and modeling of atmospheric OH and HO₂* radicals at a subtropical rural site and implications for secondary pollutantsen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.spage8147-
dc.identifier.epage8161-
dc.identifier.volume25-
dc.identifier.issue14-
dc.identifier.doi10.5194/acp-25-8147-2025-
dcterms.abstractHOx radicals (OH and HO2) are crucial oxidants that determine atmospheric oxidation capacity and the production of secondary pollutants; however, their sources and sinks remain incompletely understood in certain rural, forest, and maritime environments. This study measured HO2* (HO2 contribution from RO2, organic peroxyl radicals) and OH concentrations using a chemical ionization mass spectrometer at a subtropical rural site in southern China from 12 November to 19 December 2022. The average peak concentrations were 3.50 2.47 106cm 3 for OH and 1.34 0.93 108cm 3 for HO2*. Model-estimated contribution from RO2 to HO2 during the measurement period ranged from 44% to 69% of HO2*. Calculations based on an observationconstrained chemical model revealed an overestimation of HO2 and OH concentrations during warm periods of the field study. Sensitivity tests suggest that adding HOx sinks or an HO2 recycle process to the model could improve the model performance. Over-simulation of HOx in the model resulted in overestimations of midday (10:00–15:00UTC) production rates by more than 79% for ozone and a factor of 1.88 for nitric acid. Our study highlights the need for further improving understanding of the sources and sinks of OH and HO2 and representation of them in air quality models.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationAtmospheric chemistry and physics, 2025, v. 25, no. 14, p. 8147-8161-
dcterms.isPartOfAtmospheric chemistry and physics-
dcterms.issued2025-
dc.identifier.scopus2-s2.0-105017264359-
dc.identifier.eissn1680-7324-
dc.description.validate202511 bcch-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Scopus/WOSen_US
dc.description.fundingSourceRGCen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextThis research was financially supported by the Hong Kong Research Grants Council (T24-504/17-N and 15223221 to Tao Wang), the National Science Foundation of China (42293322 to Tao Wang), and The Hong Kong Polytechnic University Postdoc Matching Fund Scheme (P0043403 to Tianshu Chen).en_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryCCen_US
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