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AGU: Journal of Geophysical Research, Atmospheres

 

Keywords

  • CCN
  • organic aerosols
  • ozone
  • oleic acid
  • oxidative processing

Index Terms

  • Atmospheric Composition and Structure: Aerosols and particles
  • Atmospheric Composition and Structure: Cloud physics and chemistry
  • Atmospheric Composition and Structure: Pollution—urban and regional
Abstract
Cited By (7)
 

Abstract

Formation of cloud condensation nuclei by oxidative processing: Unsaturated fatty acids

Keith E. Broekhuizen

Department of Chemistry, University of Toronto, Toronto, Ontario, Canada

Troy Thornberry

NOAA Aeronomy Laboratory, Boulder, Colorado, USA

Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado, USA

P. Pradeep Kumar

Department of Physics, University of Pune, Pune, India

Jonathan P. D. Abbatt

Department of Chemistry, University of Toronto, Toronto, Ontario, Canada

The ability of submicron oleic acid and linoleic acid particles, or condensation nuclei (CN), to act as cloud condensation nuclei (CCN) has been investigated using a tandem differential mobility analyzer (TDMA) coupled to a flow tube reactor and a thermal gradient diffusion chamber (TGDC). The size change and CCN properties of pure oleic acid, mixed oleic acid/methanol, and pure linoleic acid particles have been investigated as a function of exposure to ozone. Pure oleic and linoleic acid particles were CCN inactive for all particle diameters (≤300 nm) and supersaturations (≤1%) studied. The mixed oleic acid/methanol particles, however, had a critical activation diameter of 188 nm for an experimental water supersaturation of 0.6%. Under low ozone exposures (<1 × 10−4 atm s), both the oleic acid and linoleic acid particles decreased in size. In particular, oleic acid particles lost 25% of their initial volume, consistent with the loss of nonanal, a volatile reaction product. However, no increase in CCN activity was observed at these exposures. Under conditions of much higher ozone exposure, e.g., 0.42 atm s, the pure oleic acid particles became CCN active, with a critical activation diameter of 161 nm at 0.6% supersaturation. CCN activity for the linoleic acid particles was never observed, even under these high ozone exposures not typically observed in the atmosphere. By contrast, the mixed oleic acid/methanol particles showed enhanced activation under atmospherically relevant ozone exposures (<1 × 10−4 atm s). These results suggest that the products of the ozone plus unsaturated fatty acid reaction do promote the CCN activity of the particles; however, the degree of activity is dependent on both the level of ozone exposure and the chemical nature of the particle. These results are the first to demonstrate that the CCN properties of pure organic aerosols can be modified through oxidative processing.

Received 29 July 2004; accepted 18 October 2004; published 21 December 2004.

Citation: Broekhuizen, K. E., T. Thornberry, P. P. Kumar, and J. P. D. Abbatt (2004), Formation of cloud condensation nuclei by oxidative processing: Unsaturated fatty acids, J. Geophys. Res., 109, D24206, doi:10.1029/2004JD005298.

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