Nitrate radicals suppress biogenic new particle formation from monoterpene oxidation

Author:

Li Dandan1,Huang Wei2,Wang Dongyu3,Wang Mingyi4,Thornton Joel5,Caudillo Lucía6,Rörup Birte7,Marten Ruby3,Scholz Wiebke8,Finkenzeller Henning9,Marie Guillaume6ORCID,Bell David10,Brasseur Zoé11ORCID,Curtius Joachim12ORCID,Dada Lubna3,Duplissy Jonathan2ORCID,Gong Xianda13ORCID,Hansel Armin14ORCID,He Xu-cheng7ORCID,Hofbauer Victoria15,Junninen Heikki16ORCID,Krechmer Jordan E.17,Kurten Andreas12,Lamkaddam Houssni18,LEHTIPALO Katrianne2ORCID,Lopez Brandon15,Ma Yingge19,Mahfouz Naser20ORCID,Manninen Hanna E.21,Mentler Bernhard22ORCID,Perrier Sebastien23,Petäjä Tuukka2ORCID,Pfeifer Joschka24,Philippov Maxim25ORCID,Schervish Meredith26,Schobesberger Siegfried27,Shen Jiali2,Surdu Mihnea28,Tomaz Sophie29,Volkamer Rainer9ORCID,Wang Xinke29,Weber Stefan24ORCID,Welti André30ORCID,Worsnop Douglas31,wu yusheng,Yan Chao2ORCID,Zauner-Wieczorek Marcel32ORCID,Kulmala Markku2ORCID,Kirkby Jasper33ORCID,Donahue Neil34ORCID,George Christian35ORCID,El-Haddad Imad18ORCID,Bianchi Federico2ORCID,Riva Matthieu23ORCID

Affiliation:

1. Institute of Researches on Catalysis and Environment in Lyon

2. University of Helsinki

3. Laboratory of Atmospheric Chemistry, Paul Scherrer Institute

4. Caltech

5. Department of Atmospheric Sciences, University of Washington,

6. Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main, 60438, Germany

7. Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, 00014 Helsinki, Finland

8. University of Innsbruck

9. University of Colorado Boulder

10. Pacific Northwest National Laboratory

11. Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki

12. Goethe University Frankfurt am Main

13. Washington University in St. Louis

14. Department of Ion Physics and Applied Physics, University of Innsbruck, Innsbruck

15. Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, PA, 15213, USA

16. University of Tartu

17. Aerodyne Research Incorporated, Billerica, Massachusetts

18. Paul Scherrer Institute

19. State Environmental Protection Key Laboratory of the Cause and Prevention of Urban Air Pollution Complex;Shanghai Academy of Environmental Science

20. Princeton University

21. CERN, the European Organization for Nuclear Research,

22. Institute of Ion Physics and Applied Physics, University of Innsbruck, 6020 Innsbruck, Austria

23. CNRS-IRCELYON

24. CERN, the European Organization for Nuclear Research, CH-1211 Geneva 23, Switzerland

25. P.N. Lebedev Physical Institute of the Russian Academy of Sciences, Moscow, Russia.

26. Carnegie Mellon University Center for Atmospheric Particle Studies, 5000 Forbes Ave,

27. Department of Applied Physics, University of Eastern Finland

28. Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, CH-5232 Villigen, Switzerland

29. Univ Lyon, Université Claude Bernard Lyon 1, CNRS, IRCELYON

30. National Oceanic and Atmospheric Administration

31. Aerodyne Research Inc.

32. Goethe University Frankfurt

33. CERN

34. Carnegie Mellon University

35. CNRS

Abstract

Abstract Highly oxygenated organic molecules (HOMs) are a major source of new particles affecting Earth’s climate1,2. 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 daytime3-6 than during nighttime7,8. 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 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 NO3 chemistry suppress the production of ultra-low volatility organic compounds (ULVOCs) responsible for biogenic NPF, which are covalently bound 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-rich environments.

Publisher

Research Square Platform LLC

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