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Published February 5, 2021 | Supplemental Material
Journal Article Open

Role of iodine oxoacids in atmospheric aerosol nucleation

He, Xu-Cheng ORCID icon
Tham, Yee Jun ORCID icon
Dada, Lubna ORCID icon
Wang, Mingyi ORCID icon
Finkenzeller, Henning ORCID icon
Stolzenburg, Dominik ORCID icon
Iyer, Siddharth ORCID icon
Simon, Mario ORCID icon
Kürten, Andreas ORCID icon
Shen, Jiali
Rörup, Birte ORCID icon
Rissanen, Matti ORCID icon
Schobesberger, Siegfried ORCID icon
Baalbaki, Rima ORCID icon
Wang, Dongyu S. ORCID icon
Koenig, Theodore K. ORCID icon
Jokinen, Tuija ORCID icon
Sarnela, Nina ORCID icon
Beck, Lisa J. ORCID icon
Almeida, João ORCID icon
Amanatidis, Stavros ORCID icon
Amorim, António ORCID icon
Ataei, Farnoush
Baccarini, Andrea ORCID icon
Bertozzi, Barbara ORCID icon
Bianchi, Federico ORCID icon
Brilke, Sophia ORCID icon
Caudillo, Lucía
Chen, Dexian ORCID icon
Chiu, Randall ORCID icon
Chu, Biwu ORCID icon
Dias, António ORCID icon
Ding, Aijun ORCID icon
Dommen, Josef ORCID icon
Duplissy, Jonathan ORCID icon
El Haddad, Imad ORCID icon
Gonzalez Carracedo, Loïc
Granzin, Manuel
Hansel, Armin ORCID icon
Heinritzi, Martin ORCID icon
Hofbauer, Victoria ORCID icon
Junninen, Heikki ORCID icon
Kangasluoma, Juha ORCID icon
Kemppainen, Deniz ORCID icon
Kim, Changhyuk ORCID icon
Kong, Weimeng ORCID icon
Krechmer, Jordan E. ORCID icon
Kvashin, Aleksander ORCID icon
Laitinen, Totti
Lamkaddam, Houssni ORCID icon
Lee, Chuan Ping ORCID icon
Lehtipalo, Katrianne ORCID icon
Leiminger, Markus ORCID icon
Li, Zijun ORCID icon
Makhmutov, Vladimir ORCID icon
Manninen, Hanna E. ORCID icon
Marie, Guillaume ORCID icon
Marten, Ruby ORCID icon
Mathot, Serge
Mauldin, Roy L. ORCID icon
Mentler, Bernhard ORCID icon
Möhler, Ottmar
Müller, Tatjana ORCID icon
Nie, Wei ORCID icon
Onnela, Antti ORCID icon
Petäjä, Tuukka ORCID icon
Pfeifer, Joschka ORCID icon
Philippov, Maxim ORCID icon
Ranjithkumar, Ananth ORCID icon
Saiz-Lopez, Alfonso ORCID icon
Salma, Imre ORCID icon
Scholz, Wiebke ORCID icon
Schuchmann, Simone
Schulze, Benjamin ORCID icon
Steiner, Gerhard ORCID icon
Stozhkov, Yuri ORCID icon
Tauber, Christian ORCID icon
Tomé, António ORCID icon
Thakur, Roseline C. ORCID icon
Väisänen, Olli ORCID icon
Vazquez-Pufleau, Miguel ORCID icon
Wagner, Andrea C. ORCID icon
Wang, Yonghong ORCID icon
Weber, Stefan K. ORCID icon
Winkler, Paul M. ORCID icon
Wu, Yusheng
Xiao, Mao ORCID icon
Yan, Chao ORCID icon
Ye, Qing ORCID icon
Ylisirniö, Arttu ORCID icon
Zauner-Wieczorek, Marcel ORCID icon
Zha, Qiaozhi ORCID icon
Zhou, Putian ORCID icon
Flagan, Richard C. ORCID icon
Curtius, Joachim ORCID icon
Baltensperger, Urs ORCID icon
Kulmala, Markku ORCID icon
Kerminen, Veli-Matti ORCID icon
Kurtén, Theo ORCID icon
Donahue, Neil M. ORCID icon
Volkamer, Rainer ORCID icon
Kirkby, Jasper ORCID icon
Worsnop, Douglas R. ORCID icon
Sipilä, Mikko ORCID icon

Abstract

Iodic acid (HIO₃) is known to form aerosol particles in coastal marine regions, but predicted nucleation and growth rates are lacking. Using the CERN CLOUD (Cosmics Leaving Outdoor Droplets) chamber, we find that the nucleation rates of HIO₃ particles are rapid, even exceeding sulfuric acid–ammonia rates under similar conditions. We also find that ion-induced nucleation involves IO₃⁻ and the sequential addition of HIO₃ and that it proceeds at the kinetic limit below +10°C. In contrast, neutral nucleation involves the repeated sequential addition of iodous acid (HIO₂) followed by HIO₃, showing that HIO₂ plays a key stabilizing role. Freshly formed particles are composed almost entirely of HIO₃, which drives rapid particle growth at the kinetic limit. Our measurements indicate that iodine oxoacid particle formation can compete with sulfuric acid in pristine regions of the atmosphere.

Additional Information

© 2021 American Association for the Advancement of Science. This is an article distributed under the terms of the Science Journals Default License. Received 27 July 2020; accepted 6 January 2021. We thank the European Organization for Nuclear Research (CERN) for supporting CLOUD with important technical and financial resources and for providing a particle beam from the CERN Proton Synchrotron. This research has received support from the Academy of Finland (projects 316114, 307331, 310682, 266388, 3282290, 306853, 296628, 229574, 333397, 326948, and 1325656); the European Research Council (projects 692891, 616075, 764991, 316662, 742206, and 714621); CSC – Finnish IT center; the EC Seventh Framework Programme and the EU H2020 programme Marie Skłodowska Curie ITN "CLOUD-TRAIN" (316662) and "CLOUD-MOTION" (764991); Austrian Science Fund (FWF) (J3951-N36 and P27295-N20); the Swiss National Science Foundation (20FI20_159851, 200021_169090, 200020_172602, and 20FI20_172622); the U.S. National Science Foundation (grants AGS1447056, AGS1439551, AGS1801574, AGS1620530, AGS1801897, AGS153128, AGS1649147, AGS1801280, AGS1602086, and AGS1801329); MSCA H2020 COFUND-FP-CERN-2014 fellowship (665779); German Federal Ministry of Education and Research: CLOUD-16 (01LK1601A); Portuguese Foundation for Science and Technology (CERN/FIS-COM/0014/2017); Academy of Finland Centre of Excellence in Atmospheric Sciences (grant 272041); European Regional Development Fund (project MOBTT42); Jiangsu Collaborative Innovation Center for Climate Change; Yangtze River Delta Atmosphere and Earth System Science National Observation and Research Station; Estonian Research Council (project PRG714); Hungarian National Research, Development and Innovation Office (K116788 and K132254); NASA Graduate Fellowship (NASA-NNX16AP36H); and ACTRIS 2TNA H2020 OCTAVE (654109). We are also grateful for all the people who have contributed to the field measurements around the world. Author contributions: X.-C.H., M.K., R.V., J.Ki., and M.Sip. planned the experiments. X.-C.H., Y.J.T., L.D., M.W., H.F., D.S., M.Sim., A.Kü., J.S., B.R., S.I., M.R., S.Scho., R.B., D.S.W., T.K.K., S.A., A.A., A.B., S.B., L.C., D.C., B.C., A.Dia., J.Du., I.E.H., R.C.F., L.G.C., M.G., M.H., V.H., H.J., J.Ka., D.K., C.K., W.K., J.E.K., A.Kv., T.L., H.L., C.P.L., K.L., M.L., Z.L., V.M., H.E.M., G.M., R.M., R.L.M., B.M., O.M., T.M., A.O., T.P., J.P., M.P., W.S., S.Schu., B.S., G.S., Y.S., A.T., M.V.-P., A.C.W., S.K.W., W.N., P.M.W., Y.Wu., A.Y., Y.Wang, M.Z.-W., Q.Z., J.C., M.K., U.B., R.V., J.Ki., and M.Sip. prepared the CLOUD facility or measuring instruments. X.-C.H., Y.J.T., L.D., M.W., H.F., D.S., M.Sim., J.S., B.R., M.R., R.B., D.S.W., T.K.K., T.J., N.S., L.J.B., F.A., A.B., F.B., B.B., S.B., D.C., R.C., A.Din., J.Du., L.G.C., M.G., M.H., V.H., H.J., D.K., C.K., J.E.K., H.L., C.P.L., M.L., Z.L., H.E.M., G.M., R.M., R.L.M., B.M., T.M., J.P., A.R., I.S., S.Schu., B.S., G.S., C.T., A.T., R.C.T., O.V., M.V.-P., A.C.W., S.K.W., W.N., Y.Wu, M.X., C.Y., Q.Y., A.Y., Y.Wang, M.Z.-W., R.V., and J.Ki. collected the data. X.-C.H., Y.J.T., L.D., M.W., H.F., D.S., M.Sim., J.S., B.R., R.C.F., D.K., C.K., W.K., S.K.W., P.M.W., P.Z., T.K., R.V., J.Ki, and D.R.W. analyzed the data. J.Ki. and X.-C.H. wrote the manuscript with contributions from R.V., Y.J.T., M.W., H.F., T.K.K., M.K., T.K., N.M.D., D.R.W., and M.Sip. X.-C.H., Y.J.T., L.D., M.W., H.F., D.S., B.R., S.I., M.R., S.Scho., R.B., T.K.K., N.S., A.B., A.Din., J.Do., J.Du., I.E.H., A.H., H.J., J.Ka., J.E.K., H.L., C.P.L., K.L., R.L.M., B.M., O.M., T.P., A.S.-L., I.S., P.Z., J.C., U.B., M.K., V.-M.K., T.K., N.M.D., R.V., J.Ki., D.R.W., and M.Sip. commented on and edited the manuscript. The authors declare no competing interests. Data and materials availability: Data for all figures in the main text and supplementary materials are available at the Zenodo repository (38).

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Created:
August 20, 2023
Modified:
October 20, 2023