JPL Technical Report Server

Laboratory Studies of Atmospheric Heterogeneous Chemistry

Show simple item record

dc.contributor.author Keyser, L.F. en_US
dc.contributor.author Leu, M-T. en_US
dc.date.accessioned 2004-10-06T01:51:14Z
dc.date.available 2004-10-06T01:51:14Z
dc.date.issued 1993 en_US
dc.identifier.citation Advances in Physical Chemistry en_US
dc.identifier.clearanceno 93-0592 en_US
dc.identifier.uri http://hdl.handle.net/2014/35054
dc.description.abstract In the laboratory, ice films formed by freezing from the liquid or more frequently by deposition from the vapor phase have been used to simulate stratospheric cloud surfaces for measurements of reaction and uptake rates. To obtain intrinsic surface reaction probabilities that can be used in atmospheric models, the area of the film surface that actually takes part in the reaction must be known. It is important to know not only the total surface area but also the film morphology in order to determine where and how the surface is situated and, thus, what fraction of it is available for reaction. Information on the structure of these ice films has been obtained by using several experimental methods. In the sections that follow, these methods will be discussed, then the results will be used to construct a working model of the ice films, and finally the model will be applied to an experimental study of HC1 uptake by H_2O ice. en_US
dc.format.extent 1000258 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.title Laboratory Studies of Atmospheric Heterogeneous Chemistry en_US


Files in this item

This item appears in the following Collection(s)

Show simple item record

Search


Browse

My Account