Hydroxymethanesulfonate and Sulfur(IV) in Fairbanks Winter During the ALPACA Study

dc.contributor.authorDingilian, Kayane
dc.contributor.authorHebert, Elliana
dc.contributor.authorBattaglia, Michael, Jr.
dc.contributor.authorCampbell, James R.
dc.contributor.authorCesler-Maloney, Meeta
dc.contributor.authorSimpson, William
dc.contributor.authorSt. Clair, Jason
dc.contributor.authorDibb, Jack
dc.contributor.authorTemime-Roussel, Brice
dc.contributor.authorD’Anna, Barbara
dc.contributor.authorMoon, Allison
dc.contributor.authorAlexander, Becky
dc.contributor.authorYang, Yuhan
dc.contributor.authorNenes, Athanasios
dc.contributor.authorMao, Jingqiu
dc.contributor.authorWeber, Rodney J.
dc.date.accessioned2024-06-11T15:08:44Z
dc.date.available2024-06-11T15:08:44Z
dc.date.issued2024-05-15
dc.description.abstractHydroxymethanesulfonate (HMS) in fine aerosol particles has been reported at significant concentrations along with sulfate under extreme cold conditions (-35 °C) in Fairbanks, Alaska, a high latitude city. HMS, a component of S(IV) and an adduct of formaldehyde and sulfur dioxide, forms in liquid water. Previous studies may have overestimated HMS concentrations by grouping it with other S(IV) species. In this work, we further investigate HMS and the speciation of S(IV) through the Alaskan Layered Pollution and Chemical Analysis (ALPACA) intensive study in Fairbanks. We developed a method utilizing hydrogen peroxide to isolate HMS and found that approximately 50% of S(IV) is HMS for total suspended particulates and 70% for PM2.5. The remaining unidentified S(IV) species are closely linked to HMS during cold polluted periods, showing strong increases in concentration relative to sulfate with decreasing temperature, a weak dependence on particle water, and similar particle size distributions, suggesting a common aqueous formation process. A portion of the unidentified S(IV) may originate from additional aldehyde-S(IV) adducts that are unstable in the water-based chemical analysis process, but further chemical characterization is needed. These results show the importance of organic S(IV) species in extreme cold environments that promote unique aqueous chemistry in supercooled liquid particles.
dc.description.sponsorshipWe thank the entire ALPACA science team of researchers for designing the experiment, acquiring funding, making measurements, and ongoing analysis of the results. The ALPACA project was initiated as a part of PACES under IGAC and with the support of IASC. We thank the University of Alaska Fairbanks and the Geophysical Institute for logistical support, and Fairbanks for welcoming and engaging with this research. We thank the Alaska Department of Environmental Conservation (ADEC) for data collection at the NCORE site. K.D., E. H., M.B., and R.J.W. were supported by the National Science Foundation's (NSF) Atmospheric Geoscience Program (grant no. AGS-2029730) and the NSF Navigating the New Arctic Program (grant no. NNA-1927778). M.B. was also supported by NASA (grant no. 80NSSC18K0557). M. C-M. and W.R.S. were supported by the NSF Sustainably Navigating Arctic Pollution Through Engaging Communities (SNAPTEC) Program (grant no. 1927750). J.S.C. was supported by the NSF Atmospheric Geoscience Program (grant no. AGS2029770). J.E.D. was supported by the National Science Foundation's (NSF) Atmospheric Geoscience Program (grant no. AGS-2109023). B. T-R. and B.A. were funded by the CASPA (Climate-relevant Aerosol Sources and Processes in the Arctic) project of the Agence Nationale de la Recherche (grant ANR-21-CE01-0017) and the IPEV (French Polar Institute Paul-É mile Victor). A.M and B. A. were supported by grant NA20OAR4310295NA20OAR4310295 from NOAA. A.N. was supported by the European Research Council (ERC) project “PyroTRACH” (Grant agreement No. 726165). J.R.C. and J.M. were supported by the NSF Atmospheric Geoscience Program (grant no. AGS-2029747) and the NSF Navigating the New Arctic Program (grant no. NNA-1927750).
dc.description.urihttps://pubs.acs.org/doi/full/10.1021/acsestair.4c00012
dc.format.extent14 pages
dc.genrejournal articles
dc.identifierdoi:10.13016/m29h8j-q8uf
dc.identifier.citationDingilian, Kayane, Elliana Hebert, Michael Jr. Battaglia, James R. Campbell, Meeta Cesler-Maloney, William Simpson, Jason M. St. Clair, et al. "Hydroxymethanesulfonate and Sulfur(IV) in Fairbanks Winter During the ALPACA Study." ACS ES&T Air, May 15, 2024. https://doi.org/10.1021/acsestair.4c00012.
dc.identifier.urihttps://doi.org/10.1021/acsestair.4c00012
dc.identifier.urihttp://hdl.handle.net/11603/34626
dc.language.isoen_US
dc.publisherACS
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC Faculty Collection
dc.relation.ispartofUMBC Joint Center for Earth Systems Technology (JCET)
dc.rightsCC BY 4.0 DEED Attribution 4.0 International
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.titleHydroxymethanesulfonate and Sulfur(IV) in Fairbanks Winter During the ALPACA Study
dc.typeText
dcterms.creatorhttps://orcid.org/0000-0002-9367-5749

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