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  The contribution of sulphuric acid to atmospheric particle formation and growth: a comparison between boundary layers in Northern and Central Europe

Fiedler, V., Dal Maso, M., Boy, M., Aufmhoff, H., Hoffmann, J., Schuck, T., et al. (2005). The contribution of sulphuric acid to atmospheric particle formation and growth: a comparison between boundary layers in Northern and Central Europe. Atmospheric Chemistry and Physics, 5(1), 1773-1785. Retrieved from http://www.atmos-chem-phys.net/5/1773/2005/acp-5-1773-2005.pdf.

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 Creators:
Fiedler, V.1, Author           
Dal Maso, M.2, Author
Boy, M.2, Author
Aufmhoff, H.1, Author           
Hoffmann, J.3, Author           
Schuck, T.1, Author           
Birmill, W.2, Author
Arnold, F.1, Author           
Kulmala, M.2, Author
Affiliations:
1Frank Arnold - Atmospheric Trace Gases and Ions, Research Groups, MPI for Nuclear Physics, Max Planck Society, ou_907557              
2University of Helsinki, Dept. Physical Sciences, P.O. Box 64, FIN-00014 Univ. of Helsinki, Finland Leibnitz Institute for Tropospheric Research, Permosestrasse 15, 04318 Leipzig, ou_persistent22              
3Division Prof. Dr. Klaus Blaum, MPI for Nuclear Physics, Max Planck Society, ou_904548              

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Free keywords: sulphuric acid
 Abstract: Atmospheric gaseous sulphuric acid was measured and its influence on particle formation and growth was investigated building on aerosol data. The measurements were part of the EU-project QUEST and took place at two different measurement sites in Northern and Central Europe (Hyytiälä, Finland, March-April 2003 and Heidelberg, Germany, March-April 2004). From a comprehensive data set including sulphuric acid, particle number size distributions and meteorological data, particle growth rates, particle formation rates and source rates of condensable vapors were inferred. Growth rates were determined in two different ways, from particle size distributions as well as from a so-called timeshift analysis. Moreover, correlations between sulphuric acid and particle number concentration between 3 and 6 nm were examined and the influence of air masses of different origin was investigated. Measured maximum concentrations of sulphuric acid were in the range from 1x106 to 16x106cm-3. The gaseous sulphuric acid lifetime with respect to condensation on aerosol particles ranged from 2 to 33min in Hyytiälä and from 0.5 to 8 min in Heidelberg. Most calculated values (growth rates, formation rates, vapor source rates) were considerably higher in Central Europe (Heidelberg), due to the more polluted air and higher preexistent aerosol concentrations. Close correlations between H2SO4 and nucleation mode particles (size range: 3-6 nm) were found on most days at both sites. The percentage contribution of sulphuric acid to particle growth was below 10% at both places and to initial growth below 20%. An air mass analysis indicated that at Heidelberg new particles were formed predominantly in air advected from southwesterly directions.

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Language(s): eng - English
 Dates: 2005-07-20
 Publication Status: Issued
 Pages: -
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Title: Atmospheric Chemistry and Physics
  Alternative Title : Atmos.Chem. Phy.
Source Genre: Journal
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Pages: - Volume / Issue: 5 (1) Sequence Number: - Start / End Page: 1773 - 1785 Identifier: -