The process that occurs when the vapour pressure of the saturated aqueous solution
of a substance is less than the vapour pressure of water in the ambient air. When
water vapour is collected by the pure solid compound, a mixture of the solid and liquid
or an aqueous solution of the compound forms until the substance is dissolved and
is in equilibrium with its environment; at this time the vapour pressure of water
over the aqueous solution will equal the
partial pressure of water in the atmosphere in contact with it. A crystalline
saltaerosol particle will deliquesce in the atmosphere when the
relative humidity surpasses a characteristic value, the so-called deliquescence point.
Source:
PAC, 1990, 62, 2167
(Glossary of atmospheric chemistry terms (Recommendations 1990))
on page 2183
Cite as:
IUPAC. Compendium of Chemical Terminology, 2nd ed. (the "Gold Book"). Compiled by
A. D. McNaught and A. Wilkinson. Blackwell Scientific Publications, Oxford (1997).
XML on-line corrected version: http://goldbook.iupac.org (2006-) created by M. Nic,
J. Jirat, B. Kosata; updates compiled by A. Jenkins. ISBN 0-9678550-9-8.
https://doi.org/10.1351/goldbook.