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Photo-oxidation of Aromatic Hydrocarbons Produces Low-Volatility Organic Compounds.
Wang, Mingyi; Chen, Dexian; Xiao, Mao; Ye, Qing; Stolzenburg, Dominik; Hofbauer, Victoria; Ye, Penglin; Vogel, Alexander L; Mauldin, Roy L; Amorim, Antonio; Baccarini, Andrea; Baumgartner, Bernhard; Brilke, Sophia; Dada, Lubna; Dias, António; Duplissy, Jonathan; Finkenzeller, Henning; Garmash, Olga; He, Xu-Cheng; Hoyle, Christopher R; Kim, Changhyuk; Kvashnin, Alexander; Lehtipalo, Katrianne; Fischer, Lukas; Molteni, Ugo; Petäjä, Tuukka; Pospisilova, Veronika; Quéléver, Lauriane L J; Rissanen, Matti; Simon, Mario; Tauber, Christian; Tomé, António; Wagner, Andrea C; Weitz, Lena; Volkamer, Rainer; Winkler, Paul M; Kirkby, Jasper; Worsnop, Douglas R; Kulmala, Markku; Baltensperger, Urs; Dommen, Josef; El-Haddad, Imad; Donahue, Neil M.
Afiliação
  • Wang M; Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States.
  • Chen D; Department of Chemistry, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States.
  • Xiao M; Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States.
  • Ye Q; Department of Chemical Engineering, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States.
  • Stolzenburg D; Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland.
  • Hofbauer V; Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States.
  • Ye P; Department of Chemistry, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States.
  • Vogel AL; Faculty of Physics, University of Vienna, 1090 Vienna, Austria.
  • Mauldin RL; Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States.
  • Amorim A; Department of Chemistry, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States.
  • Baccarini A; Aerodyne Research, Incorporated, Billerica, Massachusetts 01821, United States.
  • Baumgartner B; Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438, Frankfurt am Main, Germany.
  • Brilke S; Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States.
  • Dada L; Department of Chemistry, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, United States.
  • Dias A; Department of Oceanic and Atmospheric Science, University of Colorado Boulder, Boulder, Colorado 80309, United States.
  • Duplissy J; CENTRA and FCUL, University of Lisbon, 1749-016 Lisbon, Portugal.
  • Finkenzeller H; Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland.
  • Garmash O; Faculty of Physics, University of Vienna, 1090 Vienna, Austria.
  • He XC; Faculty of Physics, University of Vienna, 1090 Vienna, Austria.
  • Hoyle CR; Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, 00014 Helsinki, Finland.
  • Kim C; CENTRA and FCUL, University of Lisbon, 1749-016 Lisbon, Portugal.
  • Kvashnin A; Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, 00014 Helsinki, Finland.
  • Lehtipalo K; Helsinki Institute of Physics, University of Helsinki, 00014 Helsinki, Finland.
  • Fischer L; Department of Chemistry & CIRES, University of Colorado Boulder, Boulder, Colorado 80309, United States.
  • Molteni U; Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, 00014 Helsinki, Finland.
  • Petäjä T; Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, 00014 Helsinki, Finland.
  • Pospisilova V; Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland.
  • Quéléver LLJ; Institute for Atmospheric and Climate Science, ETH Zurich, 8092 Zurich, Switzerland.
  • Rissanen M; Division of Chemistry and Chemical Engineering, California Institute of Technology, Pasadena, California 91125, United States.
  • Simon M; Department of Environmental Engineering, Pusan National University, Busan, 46241, Republic of Korea.
  • Tauber C; Lebedev Physical Institute, 119991 Moscow, Russia.
  • Tomé A; Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, 00014 Helsinki, Finland.
  • Wagner AC; Finnish meteorological Institute, Erik Palménin aukio 1, 00560 Helsinki, Finland.
  • Weitz L; Institute for Ion Physics and Applied Physics, University of Innsbruck, 6020 Innsbruck, Austria.
  • Volkamer R; Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland.
  • Winkler PM; Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, 00014 Helsinki, Finland.
  • Kirkby J; Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland.
  • Worsnop DR; Institute for Atmospheric and Earth System Research (INAR), University of Helsinki, 00014 Helsinki, Finland.
  • Kulmala M; Aerosol Physics Laboratory, Physics Unit, Tampere University, P.O. Box 1001, Tampere 33100, Finland.
  • Baltensperger U; Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438, Frankfurt am Main, Germany.
  • Dommen J; Faculty of Physics, University of Vienna, 1090 Vienna, Austria.
  • El-Haddad I; IDL-University of Beira Interior, Covilhã 6201-001, Portugal.
  • Donahue NM; Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438, Frankfurt am Main, Germany.
Environ Sci Technol ; 54(13): 7911-7921, 2020 07 07.
Article em En | MEDLINE | ID: mdl-32515954
To better understand the role of aromatic hydrocarbons in new-particle formation, we measured the particle-phase abundance and volatility of oxidation products following the reaction of aromatic hydrocarbons with OH radicals. For this we used thermal desorption in an iodide-adduct Time-of-Flight Chemical-Ionization Mass Spectrometer equipped with a Filter Inlet for Gases and AEROsols (FIGAERO-ToF-CIMS). The particle-phase volatility measurements confirm that oxidation products of toluene and naphthalene can contribute to the initial growth of newly formed particles. Toluene-derived (C7) oxidation products have a similar volatility distribution to that of α-pinene-derived (C10) oxidation products, while naphthalene-derived (C10) oxidation products are much less volatile than those from toluene or α-pinene; they are thus stronger contributors to growth. Rapid progression through multiple generations of oxidation is more pronounced in toluene and naphthalene than in α-pinene, resulting in more oxidation but also favoring functional groups with much lower volatility per added oxygen atom, such as hydroxyl and carboxylic groups instead of hydroperoxide groups. Under conditions typical of polluted urban settings, naphthalene may well contribute to nucleation and the growth of the smallest particles, whereas the more abundant alkyl benzenes may overtake naphthalene once the particles have grown beyond the point where the Kelvin effect strongly influences the condensation driving force.
Assuntos

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Assunto principal: Compostos Orgânicos Voláteis / Hidrocarbonetos Aromáticos Idioma: En Ano de publicação: 2020 Tipo de documento: Article

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Assunto principal: Compostos Orgânicos Voláteis / Hidrocarbonetos Aromáticos Idioma: En Ano de publicação: 2020 Tipo de documento: Article