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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 4, issue 5
Atmos. Chem. Phys., 4, 1237-1253, 2004
https://doi.org/10.5194/acp-4-1237-2004
© Author(s) 2004. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
Atmos. Chem. Phys., 4, 1237-1253, 2004
https://doi.org/10.5194/acp-4-1237-2004
© Author(s) 2004. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.

  10 Aug 2004

10 Aug 2004

Ultra-violet absorption cross sections of isotopically substituted nitrous oxide species: 14N14NO, 15N14NO, 14N15NO and 15N15NO

P. von Hessberg1, J. Kaiser2,*, M. B. Enghoff1, C. A. McLinden3, S. L. Sorensen4, T. Röckmann2, and M. S. Johnson1 P. von Hessberg et al.
  • 1Department of Chemistry, University of Copenhagen, Copenhagen, Denmark
  • 2Max-Planck Institute for Nuclear Physics, Atmospheric Physics Division, Heidelberg, Germany
  • 3Air Quality Research Branch, Meteorological Service of Canada, Toronto, Ontario, Canada
  • 4Synchrotron Radiation Research, Lund University, Lund, Sweden
  • *now at Department of Geosciences, Princeton University, Princeton, New Jersey, USA

Abstract. The isotopically substituted nitrous oxide species 14N14NO, 15N14NO, 14N15NO and 15N15NO were investigated by ultra-violet (UV) absorption spectroscopy. High precision cross sections were obtained for the wavelength range 181 to 218nm at temperatures of 233 and 283K. These data are used to calculate photolytic isotopic fractionation constants as a function of wavelength. The fractionation constants were used in a three-dimensional chemical transport model in order to simulate the actual fractionation of N2O in the stratosphere, and the results were found to be in good agreement with field studies.

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