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dc.date.accessioned2021-03-24T21:23:14Z
dc.date.available2021-09-02T22:45:45Z
dc.date.created2021-01-19T14:05:13Z
dc.date.issued2020
dc.identifier.citationWang, Zelong Yuan, Bin Ye, Chenshuo Roberts, James M. Wisthaler, Armin Lin, Yi Li, Tiange Wu, Caihong Peng, Yuwen Wang, Chaomin Wang, Sihang Yang, Suxia Wang, Baolin Qi, Jipeng Wang, Chen Song, Wei Hu, Weiwei Wang, Xinming Xu, Wanyun Ma, Nan Kuang, Ye Tao, Jiangchuan Zhang, Zhanyi Su, Hang Cheng, Yafang Wang, Xuemei Shao, Min . High Concentrations of Atmospheric Isocyanic Acid (HNCO) Produced from Secondary Sources in China. Environmental Science and Technology. 2020, 54(19), 11818-11826
dc.identifier.urihttp://hdl.handle.net/10852/84744
dc.description.abstractIsocyanic acid (HNCO) is a potentially toxic atmospheric pollutant, whose atmospheric concentrations are hypothesized to be linked to adverse health effects. An earlier model study estimated that concentrations of isocyanic acid in China are highest around the world. However, measurements of isocyanic acid in ambient air have not been available in China. Two field campaigns were conducted to measure isocyanic acid in ambient air using a high-resolution time-of-flight chemical ionization mass spectrometer (ToF-CIMS) in two different environments in China. The ranges of mixing ratios of isocyanic acid are from below the detection limit (18 pptv) to 2.8 ppbv (5 min average) with the average value of 0.46 ppbv at an urban site of Guangzhou in the Pearl River Delta (PRD) region in fall and from 0.02 to 2.2 ppbv with the average value of 0.37 ppbv at a rural site in the North China Plain (NCP) during wintertime, respectively. These concentrations are significantly higher than previous measurements in North America. The diurnal variations of isocyanic acid are very similar to secondary pollutants (e.g., ozone, formic acid, and nitric acid) in PRD, indicating that isocyanic acid is mainly produced by secondary formation. Both primary emissions and secondary formation account for isocyanic acid in the NCP. The lifetime of isocyanic acid in a lower atmosphere was estimated to be less than 1 day due to the high apparent loss rate caused by deposition at night in PRD. Based on the steady state analysis of isocyanic acid during the daytime, we show that amides are unlikely enough to explain the formation of isocyanic acid in Guangzhou, calling for additional precursors for isocyanic acid. Our measurements of isocyanic acid in two environments of China provide important constraints on the concentrations, sources, and sinks of this pollutant in the atmosphere.
dc.languageEN
dc.publisherACS Publications
dc.titleHigh Concentrations of Atmospheric Isocyanic Acid (HNCO) Produced from Secondary Sources in China
dc.typeJournal article
dc.creator.authorWang, Zelong
dc.creator.authorYuan, Bin
dc.creator.authorYe, Chenshuo
dc.creator.authorRoberts, James M.
dc.creator.authorWisthaler, Armin
dc.creator.authorLin, Yi
dc.creator.authorLi, Tiange
dc.creator.authorWu, Caihong
dc.creator.authorPeng, Yuwen
dc.creator.authorWang, Chaomin
dc.creator.authorWang, Sihang
dc.creator.authorYang, Suxia
dc.creator.authorWang, Baolin
dc.creator.authorQi, Jipeng
dc.creator.authorWang, Chen
dc.creator.authorSong, Wei
dc.creator.authorHu, Weiwei
dc.creator.authorWang, Xinming
dc.creator.authorXu, Wanyun
dc.creator.authorMa, Nan
dc.creator.authorKuang, Ye
dc.creator.authorTao, Jiangchuan
dc.creator.authorZhang, Zhanyi
dc.creator.authorSu, Hang
dc.creator.authorCheng, Yafang
dc.creator.authorWang, Xuemei
dc.creator.authorShao, Min
cristin.unitcode185,15,12,62
cristin.unitnameMiljøvitenskap
cristin.ispublishedtrue
cristin.fulltextpostprint
cristin.qualitycode2
dc.identifier.cristin1874432
dc.identifier.bibliographiccitationinfo:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Environmental Science and Technology&rft.volume=54&rft.spage=11818&rft.date=2020
dc.identifier.jtitleEnvironmental Science and Technology
dc.identifier.volume54
dc.identifier.issue19
dc.identifier.startpage11818
dc.identifier.endpage11826
dc.identifier.doihttps://doi.org/10.1021/acs.est.0c02843
dc.identifier.urnURN:NBN:no-87496
dc.type.documentTidsskriftartikkel
dc.type.peerreviewedPeer reviewed
dc.source.issn0013-936X
dc.identifier.fulltextFulltext https://www.duo.uio.no/bitstream/handle/10852/84744/1/Wang%2Bet%2Bal.%2B2020.pdf
dc.type.versionAcceptedVersion


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