Published July 1989
| public
Journal Article
Water content of atmospheric aerosols
Abstract
The water content of atmospheric aerosol particles is calculated, both above and below the classic deliquescent point. The existence of water in the paniculate phase is predicted to be strongly dependent on the aerosol composition. Liquid water may constitute a significant mass fraction of the aerosol concentration at r.h. <60%.
Additional Information
© 1989 Published by Elsevier. This work was supported by the South Coast Air Quality Management District.Additional details
- Eprint ID
- 121004
- Resolver ID
- CaltechAUTHORS:20230419-898284000.14
- South Coast Air Quality Management District (SCAQMD)
- Created
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2023-04-24Created from EPrint's datestamp field
- Updated
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2023-04-24Created from EPrint's last_modified field