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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 11, issue 14
Atmos. Chem. Phys., 11, 7343–7354, 2011
https://doi.org/10.5194/acp-11-7343-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: European Integrated Project on Aerosol-Cloud-Climate and Air...

Atmos. Chem. Phys., 11, 7343–7354, 2011
https://doi.org/10.5194/acp-11-7343-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 26 Jul 2011

Research article | 26 Jul 2011

Chemical ageing and transformation of diffusivity in semi-solid multi-component organic aerosol particles

C. Pfrang1,2, M. Shiraiwa2, and U. Pöschl2 C. Pfrang et al.
  • 1University of Reading, Department of Chemistry, PO BOX 224, Whiteknights, Reading RG6 6AD, UK
  • 2Max Planck Institute for Chemistry, Biogeochemistry Department, PO BOX 3060, 55128 Mainz, Germany

Abstract. Recent experimental evidence underlines the importance of reduced diffusivity in amorphous semi-solid or glassy atmospheric aerosols. This paper investigates the impact of diffusivity on the ageing of multi-component reactive organic particles approximating atmospheric cooking aerosols. We apply and extend the recently developed KM-SUB model in a study of a 12-component mixture containing oleic and palmitoleic acids. We demonstrate that changes in the diffusivity may explain the evolution of chemical loss rates in ageing semi-solid particles, and we resolve surface and bulk processes under transient reaction conditions considering diffusivities altered by oligomerisation. This new model treatment allows prediction of the ageing of mixed organic multi-component aerosols over atmospherically relevant timescales and conditions. We illustrate the impact of changing diffusivity on the chemical half-life of reactive components in semi-solid particles, and we demonstrate how solidification and crust formation at the particle surface can affect the chemical transformation of organic aerosols.

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