Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/113246
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dc.contributorDepartment of Civil and Environmental Engineering-
dc.creatorTsiligiannis, E-
dc.creatorWu, R-
dc.creatorLee, BH-
dc.creatorSalvador, CM-
dc.creatorPriestley, M-
dc.creatorCarlsson, PTM-
dc.creatorKang, S-
dc.creatorNovelli, A-
dc.creatorVereecken, L-
dc.creatorFuchs, H-
dc.creatorMayhew, AW-
dc.creatorHamilton, JF-
dc.creatorEdwards, PM-
dc.creatorFry, JL-
dc.creatorBrownwood, B-
dc.creatorBrown, SS-
dc.creatorWild, RJ-
dc.creatorBannan, TJ-
dc.creatorCoe, H-
dc.creatorAllan, J-
dc.creatorSurratt, JD-
dc.creatorBacak, A-
dc.creatorArtaxo, P-
dc.creatorPercival, C-
dc.creatorGuo, S-
dc.creatorHu, M-
dc.creatorWang, T-
dc.creatorMentel, TF-
dc.creatorThornton, JA-
dc.creatorHallquist, M-
dc.date.accessioned2025-05-29T07:59:38Z-
dc.date.available2025-05-29T07:59:38Z-
dc.identifier.issn0094-8276-
dc.identifier.urihttp://hdl.handle.net/10397/113246-
dc.language.isoenen_US
dc.publisherWiley-Blackwell Publishing, Inc.en_US
dc.rights© 2022. The Authors.en_US
dc.rightsThis is an open access article under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/), which permits use, distribution and reproduction in any medium, provided the original work is properly cited.en_US
dc.rightsThe following publication Tsiligiannis, E., Wu, R., Lee, B. H., Salvador, C. M., Priestley, M., Carlsson, P. T. M., et al. (2022). A four carbon organonitrate as a significant product of secondary isoprene chemistry. Geophysical Research Letters, 49, e2021GL097366 is available at https://doi.org/10.1029/2021GL097366.en_US
dc.titleA four carbon organonitrate as a significant product of secondary isoprene chemistryen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume49-
dc.identifier.issue11-
dc.identifier.doi10.1029/2021GL097366-
dcterms.abstractOxidation of isoprene by nitrate radicals (NO3) or by hydroxyl radicals (OH) under high NOx conditions forms a substantial amount of organonitrates (ONs). ONs impact NOx concentrations and consequently ozone formation while also contributing to secondary organic aerosol. Here we show that the ONs with the chemical formula C4H7NO5 are a significant fraction of isoprene-derived ONs, based on chamber experiments and ambient measurements from different sites around the globe. From chamber experiments we found that C4H7NO5 isomers contribute 5%–17% of all measured ONs formed during nighttime and constitute more than 40% of the measured ONs after further daytime oxidation. In ambient measurements C4H7NO5 isomers usually dominate both nighttime and daytime, implying a long residence time compared to C5 ONs which are removed more rapidly. We propose potential nighttime sources and secondary formation pathways, and test them using a box model with an updated isoprene oxidation scheme.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationGeophysical research letters, 16 June 2022, v. 49, no. 11, e2021GL097366-
dcterms.isPartOfGeophysical research letters-
dcterms.issued2022-06-16-
dc.identifier.scopus2-s2.0-85132074163-
dc.identifier.eissn1944-8007-
dc.identifier.artne2021GL097366-
dc.description.validate202505 bcch-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Othersen_US
dc.description.fundingSourceRGCen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextThe European Research Council (ERC) (SARLEP grant agreement no. 681529); European Commission (EC) under the European Union's Horizon 2020 research and innovation program (Eurochamp 2020 grant agreement no. 730997 and FORCeS grant agreement no. 821205); Vetenskapsrådet (VR, Grant Nos. 2014–05332 and 2018–04430); Svenska Forskningsrådet Formas (Grant Nos. 2015–1537 and 2019–586); the Natural Environment Research Council for a PhD studentship as part of the PANORAMA DTPen_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryCCen_US
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