References

ACP

Atmospheric Chemistry and Physics

ACP

1680-7324

Copernicus GmbH

Göttingen, Germany

10.5194/acp-9-3209-2009

The heterogeneous reaction of hydroxyl radicals with sub-micron squalane particles: a model system for understanding the oxidative aging of ambient aerosols

Smith

J. D.

¹ Kroll

J. H.

² Cappa

C. D.

³ Che

D. L.

¹ ⁴ Liu

C. L.

¹ ⁴ Ahmed

¹ Leone

S. R.

¹ ⁴ ⁵ Worsnop

D. R.

² Wilson

K. R.

Chemical Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA

Aerosol and Cloud Chemistry, Aerodyne Research Inc., Billerica, MA 01821, USA

Department of Civil and Environmental Engineering, University of California, Davis, CA 95616, USA

Department of Chemistry, University of California, Berkeley, CA 94720, USA

Department of Physics, University of California, Berkeley, CA 94720, USA

18 05 2009

9 9 3209 3222

This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

This article is available from http://www.atmos-chem-phys.net/9/3209/2009/acp-9-3209-2009.html

The full text article is available as a PDF file from http://www.atmos-chem-phys.net/9/3209/2009/acp-9-3209-2009.pdf

The heterogeneous reaction of OH radicals with sub-micron squalane particles, in the presence of O2, is used as a model system to explore the fundamental chemical mechanisms that control the oxidative aging of organic aerosols in the atmosphere. Detailed kinetic measurements combined with elemental mass spectrometric analysis reveal that the reaction proceeds sequentially by adding an average of one oxygenated functional group per reactive loss of squalane. The reactive uptake coefficient of OH with squalane particles is determined to be 0.3±0.07 at an average OH concentration of ~1×1010 molecules cm−3. Based on a comparison between the measured particle mass and model predictions it appears that significant volatilization of a reduced organic particle would be extremely slow in the real atmosphere. However, as the aerosols become more oxygenated, volatilization becomes a significant loss channel for organic material in the particle-phase. Together these results provide a chemical framework in which to understand how heterogeneous chemistry transforms the physiochemical properties of particle-phase organic matter in the troposphere.

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