Anthropogenic organic aerosol in Europe produced mainly through second-generation oxidation

Mao Xiao, Mingyi Wang, Bernhard Mentler, Olga Garmash, Houssni Lamkaddam, Ugo Molteni, Mario Simon, Lauri Ahonen, Antonio Amorim, Andrea Baccarini, Paulus Salomon Bauer, Dexian Chen, Randall Chiu, Lubna Dada, Jonathan Duplissy, Henning Finkenzeller, Lukas Fischer, Xu Cheng He, Martin Heinritzi, Victoria HofbauerChanghyuk Kim, Andreas Kürten, Aleksandr Kvashnin, Katrianne Lehtipalo, Yuliang Liu, Huajun Mai, Vladimir Makhmutov, Serge Mathot, Roy Mauldin, Antti Onnela, Tuukka Petäjä, Lauriane L.J. Quéléver, Matti Rissanen, Simone Schuchmann, Mikko Sipilä, Dominik Stolzenburg, Yuri Stozhkov, Christian Tauber, António Tomé, Robert Wagner, Chao Yan, Boxing Yang, Penglin Ye, Qiaozi Zha, Joachim Curtius, Armin Hansel, Jasper Kirkby, Markku Kulmala, Rainer Volkamer, Paul M. Winkler, Douglas R. Worsnop, Wei Nie, Neil M. Donahue, Christopher R. Hoyle, Jianhui Jiang, Urs Baltensperger, Josef Dommen, Imad El Haddad

Research output: Contribution to journalArticlepeer-review

1 Scopus citations

Abstract

Exposure to anthropogenic atmospheric aerosol is a major health issue, causing several million deaths per year worldwide. The oxidation of aromatic hydrocarbons from traffic and wood combustion is an important anthropogenic source of low-volatility species in secondary organic aerosol, especially in heavily polluted environments. It is not yet established whether the formation of anthropogenic secondary organic aerosol involves mainly rapid autoxidation, slower sequential oxidation steps or a combination of the two. Here we reproduced a typical urban haze in the ‘Cosmics Leaving Outdoor Droplets’ chamber at the European Organization for Nuclear Research and observed the dynamics of aromatic oxidation products during secondary organic aerosol growth on a molecular level to determine mechanisms underlying their production and removal. We demonstrate that sequential oxidation is required for substantial secondary organic aerosol formation. Second-generation oxidation decreases the products’ saturation vapour pressure by several orders of magnitude and increases the aromatic secondary organic aerosol yields from a few percent to a few tens of percent at typical atmospheric concentrations. Through regional modelling, we show that more than 70% of the exposure to anthropogenic organic aerosol in Europe arises from second-generation oxidation.

Original languageEnglish
Article number4926
Pages (from-to)239-245
Number of pages7
JournalNature Geoscience
Volume18
Issue number3
DOIs
StatePublished - Mar 2025

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