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Laboratory measurements of polar stratospheric cloud rate parametersIt is now clear that heterogeneous reactions play an important role in controlling the concentration of ozone in the stratosphere. In this work, the loss of N2O5 on ice substrates has been studied in a flow reactor in an attempt to gain a more fundamental understanding of these reactions. The apparent reaction probability in this system was found to decrease as the substrate was exposed to N2O5. A model which corrected for the loss of surface sites was developed and although it appears to fit the data for a given experiment quite well, it is concluded that the loss of reactive sites is not the full explanation. In addition, the results of an experimental and modeling study suggest that reaction on the internal surface of the ice substrates is not a major loss mechanism for N2O5 in the current work.
Document ID
19950004601
Document Type
Conference Paper
Authors
Kenner, Rex D. (Commonwealth Scientific and Industrial Research Organization Linfield, Australia)
Plumb, Ian C. (Commonwealth Scientific and Industrial Research Organization Linfield, Australia)
Ryan, Keith R. (Commonwealth Scientific and Industrial Research Organization Linfield, Australia)
Date Acquired
September 6, 2013
Publication Date
April 1, 1994
Publication Information
Publication: NASA. Goddard Space Flight Center, Ozone in the Troposphere and Stratosphere, Part 2
Subject Category
GEOPHYSICS
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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