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Published July 1989 | public
Journal Article

Water content of atmospheric aerosols


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.

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