Premium
Heterogeneous nucleation of a common atmospheric aerosol: Ammonium sulfate
Author(s) -
Oatis Susan,
Imre Dan,
McGraw Robert,
Xu Jun
Publication year - 1998
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/1998gl900199
Subject(s) - efflorescence , nucleation , aerosol , metastability , impurity , chemical physics , particulates , materials science , radiative transfer , relative humidity , ammonium sulfate , particle (ecology) , atmospheric sciences , mineralogy , chemistry , thermodynamics , physics , geology , optics , organic chemistry , oceanography , metallurgy
Natural and anthropogenic aerosols have a direct impact on the earth's radiative balance. Many of the common atmospheric aerosols contain hygroscopic salts and therefore their physical state and composition are sensitive to the relative humidity. The phase of the aerosol particle will dramatically affect the relative rates of atmospheric reactions, and radiative properties such as scattering and optical activity. In order to understand these atmospheric processes and provide accurate input for global modeling, it is imperative that these phase transitions be well defined. It is thought that the degree of metastability is influenced by the presence of foreign particulate matter. These solid impurities are predicted to reduce the barrier of nucleation by providing a surface upon which heterogeneous nucleation can be catalyzed. We report the results of CaCO 3 and BaSO 4 solid impurities on the efflorescence of (NH 4 ) 2 SO 4 ‐H 2 O micro‐droplets. The results show that both solid impurities act as catalysts for heterogeneous nucleation by causing a decrease in the degree of metastability at the efflorescence point. BaSO 4 does not prove to be significantly more efficient than CaCO 3 in spite of having the same crystalline structure and similar lattice parameters as in (NH 4 ) 2 SO 4 .