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Ozone destruction on ice
Author(s) -
Langenberg Stefan,
Schurath Ulrich
Publication year - 1999
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/1999gl900325
Subject(s) - ozone , cirrus , atmospheric sciences , ozone depletion , environmental science , water ice , chemistry , meteorology , geology , astrobiology , physics
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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