Atmos. Chem. Phys. Discuss., 12, 22813-22833, 2012
www.atmos-chem-phys-discuss.net/12/22813/2012/
doi:10.5194/acpd-12-22813-2012
© Author(s) 2012. This work is distributed
under the Creative Commons Attribution 3.0 License.
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This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
Flux induced growth of atmospheric nano-particles by organic vapors
J. Wang, R. L. McGraw, and C. Kuang
Atmospheric Sciences Division, Brookhaven National Laboratory, Upton, NY 11973-5000, USA

Abstract. Atmospheric aerosols play critical roles in air quality, public health, and visibility. In addition, they strongly influence climate by scattering solar radiation and by changing the reflectivity and lifetime of clouds. One major but still poorly understood source of atmospheric aerosol is new particle formation, which consists of the formation of thermodynamically stable clusters from trace gas molecules (homogeneous nucleation) followed by growth of these clusters to a detectable size (~3 nm). Because freshly nucleated clusters are most susceptible to loss due to high rate of coagulation with pre-existing aerosol population, the initial growth rate strongly influences the rate of new particle formation and ambient aerosol population. Whereas many field observations and modeling studies indicate that organics enhance the initial growth of the clusters and therefore new particle formation, thermodynamic considerations would suggest that the strong increase of equilibrium vapor concentration due to cluster surface curvature (Kelvin effect) may prevent ambient organics from condensing on these small clusters. Here the initial condensational growth of freshly nucleated clusters is described as heterogeneous nucleation of organic molecules onto these clusters. We find that the strong gradient in cluster population with respect to its size lead to positive cluster number flux, and therefore driving the growth of clusters substantially smaller than the Kelvin diameter, conventionally considered as the minimum particle size that can be grown through condensation. The conventional approach neglects this contribution from the cluster concentration gradient, and underestimates the rate of new particle formation by a factor of up to 60.

Citation: Wang, J., McGraw, R. L., and Kuang, C.: Flux induced growth of atmospheric nano-particles by organic vapors, Atmos. Chem. Phys. Discuss., 12, 22813-22833, doi:10.5194/acpd-12-22813-2012, 2012.
 
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