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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 15, issue 16
Atmos. Chem. Phys., 15, 9327–9343, 2015
https://doi.org/10.5194/acp-15-9327-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 15, 9327–9343, 2015
https://doi.org/10.5194/acp-15-9327-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 21 Aug 2015

Research article | 21 Aug 2015

The influences of mass loading and rapid dilution of secondary organic aerosol on particle volatility

K. R. Kolesar et al.

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by K. R. Kolesar on behalf of the Authors (23 Jul 2015)  Author's response    Manuscript
ED: Publish as is (04 Aug 2015) by Annele Virtanen
Publications Copernicus
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Short summary
Secondary organic aerosol from the dark ozonolysis of α‑pinene was formed at a range of mass loadings from 1 to 800μg m-3. The amount of mass loss during evaporation in a thermodenuder was found to be independent of mass loading. A kinetic model of evaporation was fit to the observations and good agreement was obtained when the particle was either composed of dimers that decompose into semi-volatile monomers or when it was composed of low-volatility compounds that evaporate directly.
Secondary organic aerosol from the dark ozonolysis of α‑pinene was formed at a range of mass...
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