Multiphase sulfur chemistry facilitates particle growth in a cold and dark urban environment

dc.contributor.authorMao, Jingqiu
dc.contributor.authorBali, Kunal
dc.contributor.authorCampbell, James Raemond
dc.contributor.authorRobinson, Ellis Shipley
dc.contributor.authorDeCarlo, Peter F.
dc.contributor.authorIjaz, Amna
dc.contributor.authorTemime-Roussel, Brice
dc.contributor.authorBarbara, D'Anna
dc.contributor.authorKetcherside, Damien
dc.contributor.authorYokelson, Robert J.
dc.contributor.authorHu, Lu
dc.contributor.authorCesler-Maloney, Meeta
dc.contributor.authorSimpson, William
dc.contributor.authorGuo, Fangzhou
dc.contributor.authorFlynn, James
dc.contributor.authorSt. Clair, Jason
dc.contributor.authorNenes, Athanasios
dc.contributor.authorWeber, Rodney
dc.date.accessioned2025-01-08T15:08:33Z
dc.date.available2025-01-08T15:08:33Z
dc.date.issued2024-11-15
dc.description.abstractSulfate comprises an average of 20% of the ambient PM2.5 mass during the winter months in Fairbanks, based on 24-hour filter measurements. During the ALPACA 2022 field campaign (Jan 15th-Feb 28th of 2022), we deployed two aerosol mass spectrometers (AMS) and one aerosol chemical speciation monitor (ACSM) at three urban sites, combined with Scanning Mobility Particle Sizers (SMPS), to examine the evolution of aerosol composition and size distribution at a sub-hourly time scale. During an intense pollution episode with ambient temperature between -25 and -35°C, all three instruments (two AMS and one ACSM) recorded a sharp increase in sulfate mass, ranging from 5 to 40 μg/m³ within a few hours. This increase contributed up to half of the observed rise in ambient PM2.5 mass concentration and coincided with a substantial shift in the number distribution from particle sizes less than 100 nm diameter (Dp < 100 nm) to larger particles (Dp > 100 nm) with little increase in number concentration. The corresponding increase in the volume concentration and distribution shift to larger particle size suggests the secondary formation of sulfate and organic aerosol onto pre-existing aerosols. Comparing AMS-sulfate (all sulfur species) to inorganic sulfate measured by online particle-into-liquid sampler−ion chromatography (PILS-IC), we find roughly 80% of sulfate increase was due to organic sulfur, consistent with the observation of mass spectral signatures in the AMS of organosulfur compounds. The rapid formation of sulfate appears to coincide with spikes in ambient aldehyde concentrations (formaldehyde and acetaldehyde) and an increase in S(IV) in ambient PM2.5. This likely results from multiphase chemistry, where hydroxymethanesulfonate (HMS) and other aldehyde-S(IV) adducts are formed through reactions between aldehydes and SO2 in deliquesced aerosols. We estimate that all S(IV) species, including HMS, contribute an average of 30% to aerosol sulfur, with a dominant fraction occurring during rapid sulfate increase events. Our work highlights the crucial role of controlling aldehydes to mitigate severe air pollution events in Fairbanks and may apply to other urban areas. It also emphasizes the significance of multiphase chemistry in driving particle growth from Aitken mode to accumulation mode, a key step for aerosol-cloud interactions.
dc.description.sponsorshipJ.M., J.R.C. and K.B. were supported by the National Science Foundation (NSF) Atmospheric Geoscience Program (grant no. AGS-2029747) and the NSF Navigating the New Arctic Program (grant no. NNA-1927750). R.J.W. was supported by the NSF Atmospheric Geoscience Program (grant no. AGS-2029730) and the NSF Navigating the New Arctic Program (grant no. NNA1927778). F.G. and J.H.F. were supported by the NSF Atmospheric Geoscience Program (grant no. AGS-2109098). J.M.S.C. acknowledges support from the NASA Tropospheric Composition Program and the NSF Atmospheric Chemistry Program (grant no. 2029770). A.I., B.D and B.T-R were supported by the CASPA (Climate-relevant Aerosol Sources and Processes in the Arctic) project of the Agence Nationale de la Recherche (grant no. ANR-21- CE01-0017) and INSU-CNRS (National Institute of Sciences of the Universe) via its national LEFE program and IPEV (French Polar Institute Paul-Émile Victor). Funding support for E. S. R. and P. F. D. comes from the U.S. National Science Foundation's (NSF) Navigating the New Arctic (NNA) Program (grant nos. NNA-90086753 and NNA1927750). W.R.S. and M.C.-M. acknowledge support from NSF grant AGS-2109134 and NNA-1927750. L. H. and R. Y. were supported by NOAA Climate Program Office’s Atmospheric Chemistry, Carbon Cycle, and Climate program, grant number NA20OAR4310296.
dc.description.urihttps://pubs.rsc.org/en/content/articlelanding/2024/fd/d4fd00170b
dc.format.extent19 pages
dc.genrejournal articles
dc.genrepostprints
dc.identifierdoi:10.13016/m2xlwp-itit
dc.identifier.citationMao, Jingqiu, Kunal Bali, James Raemond Campbell, Ellis Shipley Robinson, Peter F. DeCarlo, Amna Ijaz, Brice Temime-Roussel, et al. “Multiphase Sulfur Chemistry Facilitates Particle Growth in a Cold and Dark Urban Environment.” Faraday Discussions, November 15, 2024. https://doi.org/10.1039/D4FD00170B.
dc.identifier.urihttps://doi.org/10.1039/D4FD00170B
dc.identifier.urihttp://hdl.handle.net/11603/37142
dc.language.isoen_US
dc.publisherRoyal Society of Chemistry
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC Faculty Collection
dc.relation.ispartofUMBC Chemistry & Biochemistry Department
dc.relation.ispartofUMBC GESTAR II
dc.relation.ispartofUMBC Joint Center for Earth Systems Technology (JCET)
dc.rightsThis item is likely protected under Title 17 of the U.S. Copyright Law. Unless on a Creative Commons license, for uses protected by Copyright Law, contact the copyright holder or the author.
dc.titleMultiphase sulfur chemistry facilitates particle growth in a cold and dark urban environment
dc.typeText
dcterms.creatorhttps://orcid.org/0000-0002-9367-5749

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