HR: 0800h
AN: A51E-0831 [Abstracts]
TI: Hygroscopicity of Biomass Burning Derived Organic Species Particles
AU: * Chan, M
EM: jtcmn@ust.hk
AF: Environmental Engineering Program, Hong Kong University of Science and Technology, Environmental
Engineering Program, School of Engineering, Hong Kong University of Science and Technology, Clear Water Bay, Kowloon, Hong
Kong, 852
Hong Kong
AU: Chan, C
EM: keckchan@ust.hk
AF: Department of Chemical Engineering, Hong Kong University of Science and Technology, Department of
Chemical Engineering, Hong Kong University of Science and Technology, Clear Water Bay, Kowloon, Hong Kong, 852
Hong Kong
AB:
Organic species derived from biomass burning can potentially affect the hygroscopicity and cloud condensation activities of
aerosols. The hygroscopicity of particles of 3 organic species most commonly detected in biomass burning aerosols
(levoglucosan, mannosan, and galactosan) were investigated. The hygroscopic measurements were performed by levitating single
particles of roughly 10 microns in diameter in an electrodynamic balance by electric fields and equilibrating the particles
at different RH for in situ relative mass determination. Levoglucosan, mannosan, and galactosan particles did not crystallize
nor deliquesce. They existed as highly concentrated liquid droplets at low RH, suggesting that biomass burning aerosols may
retain water at low RH. These particles show very similar hygroscopic growth and the RH dependence of the Gf, (the ratio of
particle diameter equilibrated at a given RH to that at the reference RH (<10%)) can be modeled by Gf = (1-RH/100)^-0.10.
Field study has shown that the light scattering coefficient of aged smoke particles was smaller than the young smoke
particles. This suggests that the aged smoke particles were less hygroscopic than young smoke particles. This observation may
due to the formation of spherical, amorphous carbonaceous particles and the rapid conversion of more hygroscopic potassium
chloride in young smoke particles to less hygroscopic potassium sulfate and potassium nitrate in aged smoke particles. In
addition, it is possible that levoglucosan can be further converted into more simple organic acids such as C2-C5 dicarboxylic
acids, which are generally less hygroscopic with Gf < 1.10 at 85%RH during the initial aging of smoke particle. It is noted
that, although malonic acid has Gf = 1.40 at 85%RH, oxalic acid is usually the most abundant dicarboxylic acids detected in
biomass burning aerosols and has a Gf = 1.08, which is less hygroscopic than levoglucosan (Gf = 1.21). These hygroscopic
results provide additional evidence that aged smoke particles may be less hygroscopic than the fresh smoke particles.
DE: 0305 Aerosols and particles (0345, 4801)
SC: Atmospheric Sciences [A]
MN: 2004 AGU Fall Meeting