HR: 1340h
AN: A23B-1257 [Abstracts]
TI: Cloud Condensation Nucleus Activity of calcite and calcite coated with model humic and fulvic
acids
AU: * Hatch, C D
EM: Courtney-Hatch@uiowa.edu
AF: University of Iowa, IATL 222, Iowa City, IA 52242, United States
AU: Gierlus, K M
EM: Kelly-Gierlus
AF: University of Iowa, IATL 222, Iowa City, IA 52242, United States
AU: Schuttlefield, J D
EM: Jennifer-Schuttlefield@uiowa.edu
AF: University of Iowa, IATL 222, Iowa City, IA 52242, United States
AU: Grassian, V H
EM: Vicki-Grassian@uiowa.edu
AF: University of Iowa, IATL 222, Iowa City, IA 52242, United States
AB:
Many recent studies have shown that organics can alter the water adsorption and cloud condensation nuclei
(CCN) activity of common deliquescent species in the Earth's atmosphere. However, very little is known about
the effect of organics on water adsorption and CCN activity of common inactive cloud nuclei, such as mineral
aerosol. As many studies have shown that a large fraction of unidentified organic material in aerosol particles is
composed of polycarboxylic acids resembling humic substances, the presence of these large molecular weight
Humic-Like Substances (HULIS) may also alter the water adsorption and CCN activity of mineral aerosol. Thus,
we have measured the water adsorption and CCN activity of model humic and fulvic acids. Additionally, the water
adsorption and CCN activity of mineral aerosol particles coated with humic and fulvic acids have been studied.
We find that humic and fulvic acids show continual multilayer water adsorption as the relative humidity is raised.
Additionally, we find that calcite particles mixed with humic and fulvic acids take up more water by mass, by a
factor of two, compared to the uncoated calcite particles at approximately 70% RH. CCN measurements also
indicate that internally mixed calcite-humic or fulvic acid aerosols are more CCN active than the otherwise
inactive, uncoated calcite particles. Our results suggest that mineral aerosol particles coated with high molecular
weight organic materials will take up more water and become more efficient CCN in the Earth's atmosphere than
single-component mineral aerosol.
DE: 0305 Aerosols and particles (0345, 4801, 4906)
DE: 0320 Cloud physics and chemistry
SC: Atmospheric Sciences [A]
MN: 2007 Fall Meeting