Chemical composition of atmospheric nanoparticles formed from nucleation in Tecamac, Mexico: Evidence for an important role for organic species in nanoparticle growth

  • J. N. Smith
    National Center for Atmospheric Research Boulder Colorado USA
  • M. J. Dunn
    National Center for Atmospheric Research Boulder Colorado USA
  • T. M. VanReken
    National Center for Atmospheric Research Boulder Colorado USA
  • K. Iida
    Department of Mechanical Engineering University of Minnesota Minneapolis Minnesota USA
  • M. R. Stolzenburg
    Department of Mechanical Engineering University of Minnesota Minneapolis Minnesota USA
  • P. H. McMurry
    Department of Mechanical Engineering University of Minnesota Minneapolis Minnesota USA
  • L. G. Huey
    School of Earth and Atmospheric Sciences Georgia Institute of Technology Atlanta Georgia USA

書誌事項

公開日
2008-02
権利情報
  • http://onlinelibrary.wiley.com/termsAndConditions#vor
DOI
  • 10.1029/2007gl032523
公開者
American Geophysical Union (AGU)

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説明

<jats:p>We report Thermal Desorption Chemical Ionization Mass Spectrometer (TDCIMS) measurements of the composition of ambient 10–33 nm diameter particles formed from nucleation on 16 March 2006 in Tecamac, Mexico during the Megacity Initiative: Local and Global Research Observations (MILAGRO) field study. On this day, nucleated particles contained far more organics than sulfates: average ion molar ratios with measurement uncertainties for nitrate, organics and sulfur species were 6 ± 2%, 84 ± 5%, and 10 ± 1%, respectively. The measured organic species include nitrogen‐containing organic compounds, organic acids, and hydroxy organic acids. Independent calculations show that sulfuric acid condensation could have accounted for only 10 ± 2% of the growth that was observed on this day, which is consistent with the TDCIMS measurements of composition. It follows that organic compounds play a dominant role the high growth rates that were observed.</jats:p>

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