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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 12, issue 10
Atmos. Chem. Phys., 12, 4647–4666, 2012
© Author(s) 2012. 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., 12, 4647–4666, 2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 25 May 2012

Research article | 25 May 2012

Aerosol charging state at an urban site: new analytical approach and implications for ion-induced nucleation

S. Gagné1,*, J. Leppä2, T. Petäjä1, M. J. McGrath1,**, M. Vana1,3, V.-M. Kerminen2, L. Laakso1,2,4, and M. Kulmala1 S. Gagné et al.
  • 1Department of Physics, University of Helsinki, P.O. Box 64, 00014 Helsinki, Finland
  • 2Finnish Meteorological Institute, Climate Change, P.O. Box 503, 00101 Helsinki, Finland
  • 3Institute of Physics, University of Tartu, Ülikooli 18, 50090 Tartu, Estonia
  • 4School of Physical and Chemical Sciences, North-West University, Private Bag x6001, Potchefstroom 2520, South Africa
  • *now at: Dept. of Physics and Atmospheric Science, Dalhousie University, Halifax, B3H 3J5, Canada and at Environment Canada, Toronto, M3H 5T4, Canada
  • **now at: Dept. of Biophysics, Graduate School of Science, Kyoto University, Sakyo Kyoto 606-8502, Japan

Abstract. The charging state of aerosol populations was determined using an Ion-DMPS in Helsinki, Finland between December 2008 and February 2010. We extrapolated the charging state and calculated the ion-induced nucleation fraction to be around 1.3 % ± 0.4 % at 2 nm and 1.3 % ± 0.5 % at 1.5 nm, on average. We present a new method to retrieve the average charging state for a new particle formation event, at a given size and polarity. We improve the uncertainty assessment and fitting technique used previously with an Ion-DMPS. We also use a new theoretical framework that allows for different concentrations of small ions for different polarities (polarity asymmetry). We extrapolate the ion-induced fraction using polarity symmetry and asymmetry. Finally, a method to calculate the growth rates from the behaviour of the charging state as a function of the particle diameter using polarity symmetry and asymmetry is presented and used on a selection of new particle formation events.

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