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AGU: Geophysical Research Letters

 

Keywords

  • N2O5
  • heterogeneous

Index Terms

  • Atmospheric Composition and Structure: Aerosols and particles
  • Atmospheric Composition and Structure: Troposphere: composition and chemistry
  • Atmospheric Composition and Structure: Chemical kinetic and photochemical properties
  • Atmospheric Composition and Structure: Pollution: urban and regional

Abstract

GEOPHYSICAL RESEARCH LETTERS, VOL. 36, L19803, 5 PP., 2009
doi:10.1029/2009GL040248

Direct observations of N2O5 reactivity on ambient aerosol particles

Timothy H. Bertram

Department of Atmospheric Sciences, University of Washington, Seattle, Washington, USA

Joel A. Thornton

Department of Atmospheric Sciences, University of Washington, Seattle, Washington, USA

Theran P. Riedel

Department of Chemistry, University of Washington, Seattle, Washington, USA

Ann M. Middlebrook

Earth System Research Laboratory, NOAA, Boulder, Colorado, USA

Roya Bahreini

Earth System Research Laboratory, NOAA, Boulder, Colorado, USA

CIRES, University of Colorado, Boulder, Colorado, USA

Timothy S. Bates

Pacific Marine Environmental Laboratory, NOAA, Seattle, Washington, USA

Patricia K. Quinn

Pacific Marine Environmental Laboratory, NOAA, Seattle, Washington, USA

Derek J. Coffman

Pacific Marine Environmental Laboratory, NOAA, Seattle, Washington, USA

N2O5 reactivity has been measured directly for the first time on ambient aerosol particles using an entrained aerosol flow reactor coupled to a custom-built chemical ionization mass spectrometer at two urban locations during summer. The observed N2O5 reactivity is a strong function of both relative humidity (RH) and particle chemical composition. We show that particulate organic mass loadings, together with ambient relative humidity, play a leading role in determining the reaction rate of N2O5 with particles. Our observed reactivity values are both more variable and, at times, as much as a factor of ten lower than currently implemented large-scale model parameterizations would predict. Such discrepancies have likely consequences for predictions of NOx availability and ozone production, and the sensitivity of these quantities to aerosol particle loadings.

Received 28 July 2009; accepted 10 September 2009; published 8 October 2009.

Citation: Bertram, T. H., J. A. Thornton, T. P. Riedel, A. M. Middlebrook, R. Bahreini, T. S. Bates, P. K. Quinn, and D. J. Coffman (2009), Direct observations of N2O5 reactivity on ambient aerosol particles, Geophys. Res. Lett., 36, L19803, doi:10.1029/2009GL040248.

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