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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 14, issue 19
Atmos. Chem. Phys., 14, 10823–10843, 2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 14, 10823–10843, 2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 15 Oct 2014

Research article | 15 Oct 2014

The link between atmospheric radicals and newly formed particles at a spruce forest site in Germany

B. Bonn1,*, E. Bourtsoukidis1,2, T. S. Sun1,2, H. Bingemer1, L. Rondo1, U. Javed2, J. Li2, R. Axinte2, X. Li3, T. Brauers3, H. Sonderfeld4,**, R. Koppmann4, A. Sogachev5, S. Jacobi6, and D. V. Spracklen7 B. Bonn et al.
  • 1Institute for Atmospheric and Environmental Sciences, Goethe University, Frankfurt, Germany
  • 2Air Chemistry Department, Max-Planck-Institute for Chemistry, Mainz, Germany
  • 3Institute for Energy and Climate Research, IEK-8, Research Center, Jülich, Germany
  • 4Physics Department, University of Wuppertal, Wuppertal, Germany
  • 5Wind Energy Department, Technical University of Denmark, Roskilde, Denmark
  • 6Hessian Agency for the Environment and Geology, Wiesbaden, Germany
  • 7Institute for Climate and Atmospheric Science, School of Earth and Environment, University of Leeds, Leeds, UK
  • *now at: Institute for Advanced Sustainability Studies, Potsdam, Germany
  • **now at: Atmospheric Chemistry Group, Department of Chemistry, University of Leicester, Leicester, UK

Abstract. It has been claimed for more than a century that atmospheric new particle formation is primarily influenced by the presence of sulfuric acid. However, the activation process of sulfuric acid related clusters into detectable particles is still an unresolved topic. In this study we focus on the PARADE campaign measurements conducted during August/September 2011 at Mt Kleiner Feldberg in central Germany. During this campaign a set of radicals, organic and inorganic compounds and oxidants and aerosol properties were measured or calculated. We compared a range of organic and inorganic nucleation theories, evaluating their ability to simulate measured particle formation rates at 3 nm in diameter (J3) for a variety of different conditions. Nucleation mechanisms involving only sulfuric acid tentatively captured the observed noon-time daily maximum in J3, but displayed an increasing difference to J3 measurements during the rest of the diurnal cycle. Including large organic radicals, i.e. organic peroxy radicals (RO2) deriving from monoterpenes and their oxidation products, in the nucleation mechanism improved the correlation between observed and simulated J3. This supports a recently proposed empirical relationship for new particle formation that has been used in global models. However, the best match between theory and measurements for the site of interest was found for an activation process based on large organic peroxy radicals and stabilised Criegee intermediates (sCI). This novel laboratory-derived algorithm simulated the daily pattern and intensity of J3 observed in the ambient data. In this algorithm organic derived radicals are involved in activation and growth and link the formation rate of smallest aerosol particles with OH during daytime and NO3 during night-time. Because the RO2 lifetime is controlled by HO2 and NO we conclude that peroxy radicals and NO seem to play an important role for ambient radical chemistry not only with respect to oxidation capacity but also for the activation process of new particle formation. This is supposed to have significant impact of atmospheric radical species on aerosol chemistry and should be taken into account when studying the impact of new particles in climate feedback cycles.

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