Nitrate radicals suppress biogenic new particle formation from monoterpene oxidation

单萜 激进的 化学 环境化学 硝酸盐 大气化学 光化学 臭氧 有机化学
作者
Dandan Li,Wei Huang,Dongyu Wang,Mingyi Wang,Joel A. Thornton,Lucía Caudillo,Birte Rörup,Ruby Marten,Wiebke Scholz,Henning Finkenzeller,Guillaume Marie,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,S. Perrier,Tuukka Petäj̈ä,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,J. Kirkby,Neil M. Donahue,Christian George,Imad El Haddad,Federico Bianchi,Matthieu Riva
出处
期刊:Research Square - Research Square
标识
DOI:10.21203/rs.3.rs-2722087/v1
摘要

Abstract Highly oxygenated organic molecules (HOMs) are a major source of new particles affecting Earth’s climate 1,2 . HOM production from the oxidation of volatile organic compounds (VOCs) occurs during both day and night, and can lead to new particle formation (NPF) 3,4 . However, NPF involving organic vapors has been reported much more often during daytime 3-6 than during nighttime 7,8 . Here, we show that the nitrate radicals (NO 3 ) - which arise predominantly at night – inhibit NPF during the oxidation of monoterpenes based on three lines of observational evidence: NPF experiments in the CLOUD chamber at CERN; radical chemistry experiments using an oxidation flow reactor; and field observations in a wetland that occasionally exhibits nocturnal NPF. Nitrooxy-peroxy radicals formed from NO 3 chemistry suppress the production of ultra-low volatility organic compounds (ULVOCs) responsible for biogenic NPF, which are covalently bound RO 2 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 NO 3 radicals, at sub parts per trillion level, suppress the NPF rate by a factor of 4. Ambient observations further confirm that when NO 3 chemistry is involved, monoterpene NPF is completely turned off. Our results explain the frequent absence of nocturnal biogenic NPF in monoterpene-rich environments.
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