Experiments were conducted in the large (600 m(3)) expansion chamber of the
Calspan Corporation to test the efficiency of selected organic aerosols as
cloud condensation nuclei (CCN). Solutions of pinonic acid WA), ammonium s
ulfate (AS) (as a benchmark), and a mixture of both were nebulized and used
for initial CCN spectra, as were products of cyclohexene and ct-pinene oxi
dation by ozone. Measurements of the resulting aerosols were made with both
particle-sizing instruments and a cloud condensation nucleus (CCN) counter
. Activated cloud drop number concentrations (CDNC) were determined during
chamber expansion by standard laser-scattering probes. The results support
the contention that the presence of sparingly soluble organic components in
aerosols significantly affect the rate at which these aerosols activate to
form cloud drops. However, even the organic aerosols eventually fully acti
vated to the extent expected due to size assuming complete solubility. It i
s only the time necessary to activate them which is altered and the atmosph
eric significance of this kinetic effect of organics is not yet clear. (C)
2001 Elsevier Science B.V. All rights reserved.