Articles | Volume 20, issue 6
https://doi.org/10.5194/acp-20-3669-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-20-3669-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Technical note
| 
26 Mar 2020
Technical note |
| 26 Mar 2020
| 26 Mar 2020
Technical note: Determination of binary gas-phase diffusion coefficients of unstable and adsorbing atmospheric trace gases at low temperature – arrested flow and twin tube method
Institut für Physikalische und Theoretische Chemie, University of Bonn, Bonn, Germany
now at: Klinik und Poliklinik für Hals-Nasen-Ohrenheilkunde/Chirurgie, University of Bonn, Bonn, Germany
Torsten Carstens
Institut für Physikalische und Theoretische Chemie, University of Bonn, Bonn, Germany
Institut für Meterologie und Klimaforschung, Karlsruher Institut für Technologie, Karlsruhe, Germany
Dirk Hupperich
Institut für Physikalische und Theoretische Chemie, University of Bonn, Bonn, Germany
Silke Schweighoefer
Institut für Physikalische und Theoretische Chemie, University of Bonn, Bonn, Germany
now at: UP GmbH, Ibbenbüren, Germany
Ulrich Schurath
Institut für Umweltphysik, University of Heidelberg, Heidelberg, Germany
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- Hydrogel Network: A Dynamic Solution for Reversible Metal Ion Valence Switching C. He et al. 10.1021/acs.chemmater.3c03284
Latest update: 13 Dec 2024
Short summary
Gas-phase diffusion is the first step for all heterogeneous reactions under atmospheric conditions. Therefore, we have used two complementary methods for the measurement of diffusion coefficients in the temperature range of 200–300 K: the arrested flow method is best suited for unstable gases (ozone, dinitrogen pentoxide, chlorine nitrate), and the twin tube method is best suited for stable but adsorbing trace gases (nitrogen dioxide, dinitrogen tetroxide).
Gas-phase diffusion is the first step for all heterogeneous reactions under atmospheric...
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