Articles | Volume 12, issue 6
Atmos. Chem. Phys., 12, 2809–2822, 2012
https://doi.org/10.5194/acp-12-2809-2012
Atmos. Chem. Phys., 12, 2809–2822, 2012
https://doi.org/10.5194/acp-12-2809-2012

Research article 16 Mar 2012

Research article | 16 Mar 2012

Reactions of H+(pyridine)m(H2O)n and H+(NH3)1(pyridine)m(H2O)n with NH3: experiments and kinetic modelling

M. J. Ryding1, Å. M. Jonsson2, A. S. Zatula3, P. U. Andersson1, and E. Uggerud3 M. J. Ryding et al.
  • 1Department of Chemistry, Atmospheric Science, University of Gothenburg, 412 96 Göteborg, Sweden
  • 2IVL Swedish Environmental Research Institute Ltd., P.O. Box 5302, 400 14 Göteborg, Sweden
  • 3Mass Spectrometry Laboratory and Centre for Theoretical and Computational Chemistry, Department of Chemistry, University of Oslo, P.O. Box 1033 Blindern, 0315 Oslo, Norway

Abstract. Reactions between pyridine containing water cluster ions, H+(pyridine)1(H2O)n, H+(pyridine)2(H2O)n and H+(NH3)1(pyridine)1(H2O)n (n up to 15) with NH3 have been studied experimentally using a quadrupole time-of-flight mass spectrometer. The product ions in the reaction between H+(pyridine)m(H2O)n (m = 1 to 2) and NH3 have been determined for the first time. It is found that the reaction mainly leads to cluster ions of the form H+(NH3)1(pyridine)m(H2O)n-x, with x = 1 or 2 depending on the initial size of the reacting cluster ion. For a given number of water molecules (from 5 to 15) in the cluster ion, rate coefficients are found to be slightly lower than those for protonated pure water clusters reacting with ammonia. The rate coefficients obtained from this study are used in a kinetic cluster ion model under tropospheric conditions. The disagreement between ambient ground level measurements and previous models are discussed in relation to the results from our model and future experimental directions are suggested.

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