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Nitrate Radicals Suppress Biogenic New Particle Formation from Monoterpene Oxidation.
Li, Dandan; Huang, Wei; Wang, Dongyu; Wang, Mingyi; Thornton, Joel A; Caudillo, Lucía; Rörup, Birte; Marten, Ruby; Scholz, Wiebke; Finkenzeller, Henning; Marie, Guillaume; Baltensperger, Urs; Bell, David M; Brasseur, Zoé; Curtius, Joachim; Dada, Lubna; Duplissy, Jonathan; Gong, Xianda; Hansel, Armin; He, Xu-Cheng; Hofbauer, Victoria; Junninen, Heikki; Krechmer, Jordan E; Kürten, Andreas; Lamkaddam, Houssni; Lehtipalo, Katrianne; Lopez, Brandon; Ma, Yingge; Mahfouz, Naser G A; Manninen, Hanna E; Mentler, Bernhard; Perrier, Sebastien; Petäjä, Tuukka; Pfeifer, Joschka; Philippov, Maxim; Schervish, Meredith; Schobesberger, Siegfried; Shen, Jiali; Surdu, Mihnea; Tomaz, Sophie; Volkamer, Rainer; Wang, Xinke; Weber, Stefan K; Welti, André; Worsnop, Douglas R; Wu, Yusheng; Yan, Chao; Zauner-Wieczorek, Marcel; Kulmala, Markku; Kirkby, Jasper.
Afiliação
  • Li D; Univ Lyon, Université Claude Bernard Lyon 1, CNRS, IRCELYON, Villeurbanne 69626, France.
  • Huang W; Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland.
  • Wang D; Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland.
  • Wang M; Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States.
  • Thornton JA; Department of Atmospheric Sciences, University of Washington, Seattle, Washington 98195, United States.
  • Caudillo L; Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main 60438, Germany.
  • Rörup B; Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland.
  • Marten R; Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland.
  • Scholz W; Institute for Ion Physics and Applied Physics, University of Innsbruck, Innsbruck 6020, Austria.
  • Finkenzeller H; Department of Chemistry & CIRES, University of Colorado Boulder, Boulder, Colorado 80309, United States.
  • Marie G; Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main 60438, Germany.
  • Baltensperger U; Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland.
  • Bell DM; Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland.
  • Brasseur Z; Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland.
  • Curtius J; Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main 60438, Germany.
  • Dada L; Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland.
  • Duplissy J; Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland.
  • Gong X; Helsinki Institute of Physics (HIP)/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland.
  • Hansel A; Leibniz Institute for Tropospheric Research, Leipzig 04318, Germany.
  • He XC; Institute for Ion Physics and Applied Physics, University of Innsbruck, Innsbruck 6020, Austria.
  • Hofbauer V; Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland.
  • Junninen H; Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States.
  • Krechmer JE; Institute of Physics, University of Tartu, Tartu 50090, Estonia.
  • Kürten A; Aerodyne Research Inc., Billerica, Massachusetts 01821, United States.
  • Lamkaddam H; Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main 60438, Germany.
  • Lehtipalo K; Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland.
  • Lopez B; Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland.
  • Ma Y; Finnish Meteorological Institute, Helsinki 00560, Finland.
  • Mahfouz NGA; Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States.
  • Manninen HE; State Environmental Protection Key Laboratory of Formation and Prevention of Urban Air Pollution Complex, Shanghai Academy of Environment Sciences, Shanghai 200233, P. R. China.
  • Mentler B; Atmospheric and Oceanic Sciences, Princeton University, Princeton, New Jersey 08540, United States.
  • Perrier S; CERN, the European Organization for Nuclear Research, Geneve 23 CH-1211, Switzerland.
  • Petäjä T; Institute for Ion Physics and Applied Physics, University of Innsbruck, Innsbruck 6020, Austria.
  • Pfeifer J; Univ Lyon, Université Claude Bernard Lyon 1, CNRS, IRCELYON, Villeurbanne 69626, France.
  • Philippov M; Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland.
  • Schervish M; CERN, the European Organization for Nuclear Research, Geneve 23 CH-1211, Switzerland.
  • Schobesberger S; P.N. Lebedev Physical Institute of the Russian Academy of Sciences, Moscow 119991, Russia.
  • Shen J; Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States.
  • Surdu M; Department of Applied Physics, University of Eastern Finland, Kuopio 70211, Finland.
  • Tomaz S; Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland.
  • Volkamer R; Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen 5232, Switzerland.
  • Wang X; Univ Lyon, Université Claude Bernard Lyon 1, CNRS, IRCELYON, Villeurbanne 69626, France.
  • Weber SK; Department of Chemistry & CIRES, University of Colorado Boulder, Boulder, Colorado 80309, United States.
  • Welti A; Univ Lyon, Université Claude Bernard Lyon 1, CNRS, IRCELYON, Villeurbanne 69626, France.
  • Worsnop DR; Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, Frankfurt am Main 60438, Germany.
  • Wu Y; CERN, the European Organization for Nuclear Research, Geneve 23 CH-1211, Switzerland.
  • Yan C; Finnish Meteorological Institute, Helsinki 00560, Finland.
  • Zauner-Wieczorek M; Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland.
  • Kulmala M; Aerodyne Research Inc., Billerica, Massachusetts 01821, United States.
  • Kirkby J; Institute for Atmospheric and Earth System Research/Physics, Faculty of Science, University of Helsinki, Helsinki 00014, Finland.
Environ Sci Technol ; 58(3): 1601-1614, 2024 Jan 23.
Article em En | MEDLINE | ID: mdl-38185880
ABSTRACT
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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Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Assunto principal: Ozônio / Poluentes Atmosféricos / Compostos Orgânicos Voláteis / Monoterpenos Bicíclicos Idioma: En Revista: Environ Sci Technol Ano de publicação: 2024 Tipo de documento: Article País de afiliação: França

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Assunto principal: Ozônio / Poluentes Atmosféricos / Compostos Orgânicos Voláteis / Monoterpenos Bicíclicos Idioma: En Revista: Environ Sci Technol Ano de publicação: 2024 Tipo de documento: Article País de afiliação: França