Article

Journal of Atmospheric Chemistry

, Volume 44, Issue 2, pp 171-190

A Coupled Hydrophobic-Hydrophilic Model for Predicting Secondary Organic Aerosol Formation

  • Robert J. GriffinAffiliated withDepartment of Civil and Environmental Engineering, Duke University
  • , Khoi NguyenAffiliated withDepartment of Mechanical and Aerospace Engineering, University of California at Irvine
  • , Donald DabdubAffiliated withDepartment of Mechanical and Aerospace Engineering, University of California at Irvine
  • , John H. SeinfeldAffiliated withDepartment of Chemical Engineering and Division of Engineering and Applied Science, California Institute of Technology

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Abstract

The formation of secondary organic aerosol (SOA) results from the absorption of gas-phase organic oxidation products by airborne aerosol. Historically, modeling the formation of SOA has relied on relatively crude estimates of the capability of given parent hydrocarbons to form SOA. In more recent work, surrogate organic oxidation products have been separated into two groups, hydrophobic and hydrophilic, depending on whether the product is more likely to dissolve into an organic or an aqueous phase, respectively. The surrogates are then allowed to partition only via the dominant mechanism, governed by molecular properties of the surrogate molecules. The distinction between hydrophobic and hydrophilic is based on structural and physical characteristics of the compound. In general, secondary oxidation products, because of low vapor pressures and high polarities, express affinity for both the organic and aqueous aerosol phases. A fully coupled hydrophobic-hydrophilic organic gas-particle partitioning model is presented here. The model concurrently achieves mass conservation, equilibrium between the gas phase and the organic aerosol phase, equilibrium between the gas phase and the aqueous aerosol phase, and equilibrium between molecular and ionic forms of the partitioning species in the aqueous phase. Simulations have been performed using both a zero-dimensional model and the California Institute of Technology three-dimensional atmospheric chemical transport model. Simultaneous partitioning of species by both mechanisms typically leads to a shift in the distribution of products to the organic aerosol phase and an increase in the total amount of SOA predicted as compared to previous work in which partitioning is assumed to occur independently to organic and aqueous phases.

absorption dissolution equilibrium model organic aerosol