Ozone destruction on ice
The destruction of ozone on ice surfaces was studied with an ice-coated fused silica column used as a very long flow tube. Ozone destruction was found to be very slow. At 223 K and 258 K the measured reaction probabilities fall in the range 2 × 10−8 - 4 × 10−10, decreasing with increasing ozone conc...
Gespeichert in:
| Hauptverfasser: | , |
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| Dokumenttyp: | Article (Journal) |
| Sprache: | Englisch |
| Veröffentlicht: |
15 June 1999
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| In: |
Geophysical research letters
Year: 1999, Jahrgang: 26, Heft: 12, Pages: 1695-1698 |
| ISSN: | 1944-8007 |
| DOI: | 10.1029/1999GL900325 |
| Online-Zugang: | Verlag, lizenzpflichtig, Volltext: https://doi.org/10.1029/1999GL900325 Verlag, lizenzpflichtig, Volltext: https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/1999GL900325 
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| Verfasserangaben: | Stefan Langenberg, Ulrich Schurath |
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| 520 | |a The destruction of ozone on ice surfaces was studied with an ice-coated fused silica column used as a very long flow tube. Ozone destruction was found to be very slow. At 223 K and 258 K the measured reaction probabilities fall in the range 2 × 10−8 - 4 × 10−10, decreasing with increasing ozone concentration (20-1000 nbar). The observed kinetics are explained by an at least two step mechanism. The low reaction rates observed are insignificant for ozone destruction in cirrus clouds. | ||
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