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Effect of dimethylamine on the gas phase sulfuric acid concentration measured by Chemical Ionization Mass Spectrometry.
Rondo, L; Ehrhart, S; Kürten, A; Adamov, A; Bianchi, F; Breitenlechner, M; Duplissy, J; Franchin, A; Dommen, J; Donahue, N M; Dunne, E M; Flagan, R C; Hakala, J; Hansel, A; Keskinen, H; Kim, J; Jokinen, T; Lehtipalo, K; Leiminger, M; Praplan, A; Riccobono, F; Rissanen, M P; Sarnela, N; Schobesberger, S; Simon, M; Sipilä, M; Smith, J N; Tomé, A; Tröstl, J; Tsagkogeorgas, G; Vaattovaara, P; Winkler, P M; Williamson, C; Wimmer, D; Baltensperger, U; Kirkby, J; Kulmala, M; Petäjä, T; Worsnop, D R; Curtius, J.
Afiliação
  • Rondo L; Institute for Atmospheric and Environmental Sciences Goethe University Frankfurt am Main Frankfurt am Main Germany.
  • Ehrhart S; CERN Geneva Switzerland.
  • Kürten A; Institute for Atmospheric and Environmental Sciences Goethe University Frankfurt am Main Frankfurt am Main Germany.
  • Adamov A; Department of Physics University of Helsinki Helsinki Finland.
  • Bianchi F; Laboratory of Atmospheric Chemistry Paul Scherrer Institute Villigen Switzerland; Institute for Atmospheric and Climate Science ETH Zurich Zurich Switzerland.
  • Breitenlechner M; Institute for Ion Physics and Applied Physics University of Innsbruck Innsbruck Austria.
  • Duplissy J; Department of Physics University of Helsinki Helsinki Finland.
  • Franchin A; Department of Physics University of Helsinki Helsinki Finland.
  • Dommen J; Laboratory of Atmospheric Chemistry Paul Scherrer Institute Villigen Switzerland.
  • Donahue NM; Center for Atmospheric Particle Studies Carnegie Mellon University Pittsburgh Pennsylvania USA.
  • Dunne EM; Kuopio Unit Finnish Meteorological Institute Kuopio Finland; School of Earth and Environment University of Leeds Leeds UK.
  • Flagan RC; Division of Chemistry and Chemical Engineering California Institute of Technology Pasadena California USA.
  • Hakala J; Department of Physics University of Helsinki Helsinki Finland.
  • Hansel A; Institute for Ion Physics and Applied Physics University of Innsbruck Innsbruck Austria.
  • Keskinen H; Department of Physics University of Helsinki Helsinki Finland; Department of Applied Physics University of Eastern Finland Kuopio Finland.
  • Kim J; Department of Applied Physics University of Eastern Finland Kuopio Finland.
  • Jokinen T; Department of Physics University of Helsinki Helsinki Finland.
  • Lehtipalo K; Department of Physics University of Helsinki Helsinki Finland.
  • Leiminger M; Institute for Atmospheric and Environmental Sciences Goethe University Frankfurt am Main Frankfurt am Main Germany.
  • Praplan A; Department of Physics University of Helsinki Helsinki Finland; Kuopio Unit Finnish Meteorological Institute Kuopio Finland.
  • Riccobono F; Laboratory of Atmospheric Chemistry Paul Scherrer Institute Villigen Switzerland.
  • Rissanen MP; Department of Physics University of Helsinki Helsinki Finland.
  • Sarnela N; Department of Physics University of Helsinki Helsinki Finland.
  • Schobesberger S; Department of Physics University of Helsinki Helsinki Finland; Department of Atmospheric Sciences University of Washington Seattle Washington USA.
  • Simon M; Institute for Atmospheric and Environmental Sciences Goethe University Frankfurt am Main Frankfurt am Main Germany.
  • Sipilä M; Department of Physics University of Helsinki Helsinki Finland.
  • Smith JN; Department of Applied Physics University of Eastern Finland Kuopio Finland; Department of Chemistry University of California Irvine California USA.
  • Tomé A; CENTRA-SIM University of Lisbon and University of Beira Interior Lisbon Portugal.
  • Tröstl J; Laboratory of Atmospheric Chemistry Paul Scherrer Institute Villigen Switzerland.
  • Tsagkogeorgas G; Leibniz Institute for Tropospheric Research Leipzig Germany.
  • Vaattovaara P; Department of Applied Physics University of Eastern Finland Kuopio Finland; Department of Environmental Science University of Eastern Finland Kuopio Finland.
  • Winkler PM; Faculty of Physics University of Vienna Vienna Austria.
  • Williamson C; Institute for Atmospheric and Environmental Sciences Goethe University Frankfurt am Main Frankfurt am Main Germany.
  • Wimmer D; Department of Physics University of Helsinki Helsinki Finland.
  • Baltensperger U; Laboratory of Atmospheric Chemistry Paul Scherrer Institute Villigen Switzerland.
  • Kirkby J; Institute for Atmospheric and Environmental Sciences Goethe University Frankfurt am Main Frankfurt am Main Germany; CERN Geneva Switzerland.
  • Kulmala M; Department of Physics University of Helsinki Helsinki Finland.
  • Petäjä T; Department of Physics University of Helsinki Helsinki Finland.
  • Worsnop DR; Department of Physics University of Helsinki Helsinki Finland; Aerodyne Research, Inc. Billerica Massachusetts USA.
  • Curtius J; Institute for Atmospheric and Environmental Sciences Goethe University Frankfurt am Main Frankfurt am Main Germany.
J Geophys Res Atmos ; 121(6): 3036-3049, 2016 03 27.
Article em En | MEDLINE | ID: mdl-27610289
ABSTRACT
Sulfuric acid is widely recognized as a very important substance driving atmospheric aerosol nucleation. Based on quantum chemical calculations it has been suggested that the quantitative detection of gas phase sulfuric acid (H2SO4) by use of Chemical Ionization Mass Spectrometry (CIMS) could be biased in the presence of gas phase amines such as dimethylamine (DMA). An experiment (CLOUD7 campaign) was set up at the CLOUD (Cosmics Leaving OUtdoor Droplets) chamber to investigate the quantitative detection of H2SO4 in the presence of dimethylamine by CIMS at atmospherically relevant concentrations. For the first time in the CLOUD experiment, the monomer sulfuric acid concentration was measured by a CIMS and by two CI-APi-TOF (Chemical Ionization-Atmospheric Pressure interface-Time Of Flight) mass spectrometers. In addition, neutral sulfuric acid clusters were measured with the CI-APi-TOFs. The CLOUD7 measurements show that in the presence of dimethylamine (<5 to 70 pptv) the sulfuric acid monomer measured by the CIMS represents only a fraction of the total H2SO4, contained in the monomer and the clusters that is available for particle growth. Although it was found that the addition of dimethylamine dramatically changes the H2SO4 cluster distribution compared to binary (H2SO4-H2O) conditions, the CIMS detection efficiency does not seem to depend substantially on whether an individual H2SO4 monomer is clustered with a DMA molecule. The experimental observations are supported by numerical simulations based on A Self-contained Atmospheric chemistry coDe coupled with a molecular process model (Sulfuric Acid Water NUCleation) operated in the kinetic limit.
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Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Idioma: En Revista: J Geophys Res Atmos Ano de publicação: 2016 Tipo de documento: Article

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Idioma: En Revista: J Geophys Res Atmos Ano de publicação: 2016 Tipo de documento: Article