Xu-Cheng He, Mario Simon, Siddharth Iyer, Hong-Bin Xie, Birte Rörup, Jiali Shen, Henning Finkenzeller, Dominik Stolzenburg, Rongjie Zhang, Andrea Baccarini, Yee Jun Tham, Mingyi Wang, Stavros Amanatidis, Ana A Piedehierro, Antonio Amorim, Rima Baalbaki, Zoé Brasseur, Lucía Caudillo, Biwu Chu, Lubna Dada, Jonathan Duplissy, Imad El Haddad, Richard C Flagan, Manuel Granzin, Armin Hansel, Martin Heinritzi, Victoria Hofbauer, Tuija Jokinen, Deniz Kemppainen, Weimeng Kong, Jordan Krechmer, Andreas Kürten, Houssni Lamkaddam, Brandon Lopez, Fangfang Ma, Naser G A Mahfouz, Vladimir Makhmutov, Hanna E Manninen, Guillaume Marie, Ruby Marten, Dario Massabò, Roy L Mauldin, Bernhard Mentler, Antti Onnela, Tuukka Petäjä, Joschka Pfeifer, Maxim Philippov, Ananth Ranjithkumar, Matti P Rissanen, Siegfried Schobesberger, Wiebke Scholz, Benjamin Schulze, Mihnea Surdu, Roseline C Thakur, António Tomé, Andrea C Wagner, Dongyu Wang, Yonghong Wang, Stefan K Weber, André Welti, Paul M Winkler, Marcel Zauner-Wieczorek, Urs Baltensperger, Joachim Curtius, Theo Kurtén, Douglas R Worsnop, Rainer Volkamer, Katrianne Lehtipalo, Jasper Kirkby, Neil M Donahue, Mikko Sipilä, Markku Kulmala
The main nucleating vapor in the atmosphere is thought to be sulfuric acid (H2 SO4 ), stabilized by ammonia (NH3 ). However, in marine and polar regions, NH3 is generally low, and H2 SO4 is frequently found together with iodine oxoacids [HIO x , i.e., iodic acid (HIO3 ) and iodous acid (HIO2 )]. In experiments performed with the CERN CLOUD (Cosmics Leaving OUtdoor Droplets) chamber, we investigated the interplay of H2 SO4 and HIO x during atmospheric particle nucleation. We found that HIO x greatly enhances H2 SO4 (-NH3 ) nucleation through two different interactions...
December 15, 2023: Science