Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/101867
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dc.contributorDepartment of Civil and Environmental Engineeringen_US
dc.creatorXia, Men_US
dc.creatorWang, Ten_US
dc.creatorWang, Zen_US
dc.creatorChen, Yen_US
dc.creatorPeng, Xen_US
dc.creatorHuo, Yen_US
dc.creatorWang, Wen_US
dc.creatorYuan, Qen_US
dc.creatorJiang, Yen_US
dc.creatorGuo, Hen_US
dc.creatorLau, Cen_US
dc.creatorLeung, Ken_US
dc.creatorYu, Aen_US
dc.creatorLee, Sen_US
dc.date.accessioned2023-09-20T04:40:59Z-
dc.date.available2023-09-20T04:40:59Z-
dc.identifier.urihttp://hdl.handle.net/10397/101867-
dc.language.isoenen_US
dc.publisherAmerican Chemical Societyen_US
dc.rights© 2022 American Chemical Societyen_US
dc.rightsThis document is the Accepted Manuscript version of a Published Work that appeared in final form in Environmental Science & Technology Letters, copyright © American Chemical Society after peer review and technical editing by the publisher. To access the final edited and published work see https://doi.org/10.1021/acs.est.2c02434.en_US
dc.subjectMolecular bromineen_US
dc.subjectAnthropogenic pollutionen_US
dc.subjectSea spraysen_US
dc.subjectAtmospheric oxidationen_US
dc.subjectMercuryen_US
dc.subjectAir qualityen_US
dc.titlePollution-derived Br₂ boosts oxidation power of the coastal atmosphereen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.spage12055en_US
dc.identifier.epage12065en_US
dc.identifier.volume56en_US
dc.identifier.issue17en_US
dc.identifier.doi10.1021/acs.est.2c02434en_US
dcterms.abstractThe bromine atom (Br•) has been known to destroy ozone (O3) and accelerate the deposition of toxic mercury (Hg). However, its abundance and sources outside the polar regions are not well-known. Here, we report significant levels of molecular bromine (Br2)─a producer of Br•─observed at a coastal site in Hong Kong, with an average noontime mixing ratio of 5 ppt. Given the short lifetime of Br2 (∼1 min at noon), this finding reveals a large Br2 daytime source. On the basis of laboratory and field evidence, we show that the observed daytime Br2 is generated by the photodissociation of particulate nitrate (NO3–) and that the reactive uptake of dinitrogen pentoxide (N2O5) on aerosols is an important nighttime source. Model-calculated Br• concentrations are comparable with that of the OH radical─the primary oxidant in the troposphere, accounting for 24% of the oxidation of isoprene, a 13% increase in net O3 production, and a nearly 10-fold increase in the production rate of toxic HgII. Our findings reveal that reactive bromines play a larger role in the atmospheric chemistry and air quality of polluted coastal and maritime areas than previously thought. Our results also suggest that tightening the control of emissions of two conventional pollutants (NOx and SO2)─thereby decreasing the levels of nitrate and aerosol acidity─would alleviate halogen radical production and its adverse impact on air quality.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationEnvironmental science and technology letters, 6 Sept 2022, v. 56, no. 17, p. 12055-12065en_US
dcterms.isPartOfEnvironmental science and technology lettersen_US
dcterms.issued2022-09-
dc.identifier.eissn2328-8930en_US
dc.description.validate202309 bcchen_US
dc.description.oaAccepted Manuscripten_US
dc.identifier.FolderNumbera2445-n01; a3400-n03-
dc.description.fundingSourceRGCen_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryGreen (AAM)en_US
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