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Nitrate Radicals Suppress Biogenic New Particle Formation from Monoterpene Oxidation

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posted on 2024-01-08, 05:45 authored by Dandan Li, Wei Huang, Dongyu Wang, Mingyi Wang, Joel A. Thornton, Lucía Caudillo, Birte Rörup, Ruby Marten, Wiebke Scholz, Henning Finkenzeller, Guillaume Marie, Urs Baltensperger, David M. Bell, Zoé Brasseur, Joachim Curtius, Lubna Dada, Jonathan Duplissy, Xianda Gong, Armin Hansel, Xu-Cheng He, Victoria Hofbauer, Heikki Junninen, Jordan E. Krechmer, Andreas Kürten, Houssni Lamkaddam, Katrianne Lehtipalo, Brandon Lopez, Yingge Ma, Naser G. A. Mahfouz, Hanna E. Manninen, Bernhard Mentler, Sebastien Perrier, Tuukka Petäjä, Joschka Pfeifer, Maxim Philippov, Meredith Schervish, Siegfried Schobesberger, Jiali Shen, Mihnea Surdu, Sophie Tomaz, Rainer Volkamer, Xinke Wang, Stefan K. Weber, André Welti, Douglas R. Worsnop, Yusheng Wu, Chao Yan, Marcel Zauner-Wieczorek, Markku Kulmala, Jasper Kirkby, Neil M. Donahue, Christian George, Imad El-Haddad, Federico Bianchi, Matthieu Riva
Highly oxygenated organic molecules (HOMs) are a major source of new particles that affect the Earth’s climate. HOM production from the oxidation of volatile organic compounds (VOCs) occurs during both the day and night and can lead to new particle formation (NPF). However, NPF involving organic vapors has been reported much more often during the daytime than during nighttime. Here, we show that the nitrate radicals (NO3), which arise predominantly at night, inhibit NPF during the oxidation of monoterpenes based on three lines of observational evidence: NPF experiments in the CLOUD (Cosmics Leaving OUtdoor Droplets) chamber at CERN (European Organization for Nuclear Research), radical chemistry experiments using an oxidation flow reactor, and field observations in a wetland that occasionally exhibits nocturnal NPF. Nitrooxy-peroxy radicals formed from NO3 chemistry suppress the production of ultralow-volatility organic compounds (ULVOCs) responsible for biogenic NPF, which are covalently bound peroxy radical (RO2) dimer association products. The ULVOC yield of α-pinene in the presence of NO3 is one-fifth of that resulting from ozone chemistry alone. Even trace amounts of NO3 radicals, at sub-parts per trillion level, suppress the NPF rate by a factor of 4. Ambient observations further confirm that when NO3 chemistry is involved, monoterpene NPF is completely turned off. Our results explain the frequent absence of nocturnal biogenic NPF in monoterpene (α-pinene)-rich environments.

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