Enhanced secondary organic aerosol formation due to water uptake by fine particles

Enhanced secondary organic aerosol formation due to water uptake by fine particles

[1] This study characterizes the partitioning behavior of a significant fraction of the ambient organic aerosol through simultaneous measurements of gas and particle watersoluble organic carbon (WSOC). During the summer in Atlanta, WSOC gas/particle partitioning showed a strong RH dependence that was attributed to particulate liquid water. At elevated RH levels (> 70%), a significant increase i...

Secondary organic aerosol formation

Introduction Conclusions References

Competition between water uptake and ice nucleation by glassy organic aerosol particles

Organic aerosol particles play a key role in climate by serving as nuclei for clouds and precipitation. Their sources and composition are highly variable, and their phase state ranges from liquid to solid under atmospheric conditions, affecting the pathway of activation to cloud droplets and ice crystals. Due to slow diffusion of water in the particle phase, organic particles may deviate in pha...

Secondary organic aerosol formation from biomass burning

Secondary organic aerosol formation from aromatics

Secondary organic aerosol formation from m-xylene, toluene, and benzene N. L. Ng, J. H. Kroll, A. W. H. Chan, P. S. Chhabra, R. C. Flagan, and J. H. Seinfeld Departments of Chemical Engineering and Environmental Science and Engineering, California Institute of Technology, Pasadena, CA 91125, USA current address: Aerodyne Research, Inc. 45 Manning Road, Billerica, MA 01821, USA Received: 1 March...