Atmos. Chem. Phys. Discuss., 10, 17435-17466, 2010
www.atmos-chem-phys-discuss.net/10/17435/2010/
doi:10.5194/acpd-10-17435-2010
© Author(s) 2010. This work is distributed
under the Creative Commons Attribution 3.0 License.
Review Status
This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
Measurement of the ambient organic aerosol volatility distribution: application during the Finokalia Aerosol Measurement Experiment (FAME-2008)
B. H. Lee1, E. Kostenidou2,3, L. Hildebrandt1, I. Riipinen1,4, G. J. Engelhart1, C. Mohr5, P. F. DeCarlo5, N. Mihalopoulos6, A. S. H. Prevot5, U. Baltensperger5, and S. N. Pandis1,2,3
1Department of Chemical Engineering, Carnegie Mellon University, Pittsburgh, PA, USA
2Department of Chemical Engineering, University of Patras, Patra, Greece
3Inst. of Chemical Eng. and High Temperature Chemical Processes, ICE-HT, Patra, Greece
4Department of Physics, University of Helsinki, Helsinki, Finland
5Paul Scherrer Institute, Laboratory of Atmospheric Chemistry, 5232 Villigen, Switzerland
6University of Crete, Department of Chemistry, Heraklion, Greece

Abstract. A variable residence time thermodenuder (TD) was combined with an Aerodyne Aerosol Mass Spectrometer (AMS) and a Scanning Mobility Particle Sizer (SMPS) to measure the volatility distribution of aged organic aerosol in the Eastern Mediterranean during the Finokalia Aerosol Measurement Experiment in May of 2008 (FAME-2008). A new method for the quantification of the organic aerosol volatility distribution was developed combining measurements of all three instruments together with an aerosol dynamics model.

Challenges in the interpretation of ambient thermodenuder-AMS measurements include the potential resistances to mass transfer during particle evaporation, the effects of particle size on the evaporated mass fraction, the changes in the AMS collection efficiency and particle density as the particles evaporate partially in the TD, and finally potential losses inside the TD. Our proposed measurement and data analysis method accounts for all of these problems combining the AMS and SMPS measurements.

The AMS collection efficiency of the aerosol that passed through the TD was found to be approximately 10% lower than the collection efficiency of the aerosol that passed through the bypass. The organic aerosol measured at Finokalia is approximately 2 orders of magnitude less volatile than fresh laboratory-generated biogenic secondary organic aerosol. This low volatility is consistent with its highly oxygenated AMS mass spectrum. The results are found to be highly sensitive to the mass accommodation coefficient of the evaporating species.


Citation: Lee, B. H., Kostenidou, E., Hildebrandt, L., Riipinen, I., Engelhart, G. J., Mohr, C., DeCarlo, P. F., Mihalopoulos, N., Prevot, A. S. H., Baltensperger, U., and Pandis, S. N.: Measurement of the ambient organic aerosol volatility distribution: application during the Finokalia Aerosol Measurement Experiment (FAME-2008), Atmos. Chem. Phys. Discuss., 10, 17435-17466, doi:10.5194/acpd-10-17435-2010, 2010.
 
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