4.7 Article

Estimation of secondary organic aerosol viscosity from explicit modeling of gas-phase oxidation of isoprene and α-pinene

Journal

ATMOSPHERIC CHEMISTRY AND PHYSICS
Volume 21, Issue 13, Pages 10199-10213

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/acp-21-10199-2021

Keywords

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Funding

  1. National Science Foundation [AGS-1654104]
  2. U.S. Department of Energy [DE-SC0018349]
  3. Campus France (Make Our Planet Great Again (MOPGA) short stay program grant)
  4. U.S. Department of Energy (DOE) [DE-SC0018349] Funding Source: U.S. Department of Energy (DOE)

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This study utilized the GECKO-A model to conduct explicit chemical modeling of SOA formation, investigating the effects of chemical composition, relative humidity, and other factors on particle viscosity. The simulation results showed good agreement with measurements for isoprene SOA viscosity, while underestimating the viscosity of ff-pinene SOA. The study suggests that missing processes in the model and kinetic limitations may play a role in enhancing particle viscosity.
Secondary organic aerosols (SOA) are major components of atmospheric fine particulate matter, affecting climate and air quality. Mounting evidence exists that SOA can adopt glassy and viscous semisolid states, impacting formation and partitioning of SOA. In this study, we apply the GECKO-A (Generator of Explicit Chemistry and Kinetics of Organics in the Atmosphere) model to conduct explicit chemical modeling of isoprene photooxidation and alpha-pinene ozonolysis and their subsequent SOA formation. The detailed gas-phase chemical schemes from GECKO-A are implemented into a box model and coupled to our recently developed glass transition temperature parameterizations, allowing us to predict SOA viscosity. The effects of chemical composition, relative humidity, mass loadings and mass accommodation on particle viscosity are investigated in comparison with measurements of SOA viscosity. The simulated viscosity of isoprene SOA agrees well with viscosity measurements as a function of relative humidity, while the model underestimates viscosity of ff-pinene SOA by a few orders of magnitude. This difference may be due to missing processes in the model, including autoxidation and particlephase reactions, leading to the formation of high-molar-mass compounds that would increase particle viscosity. Additional simulations imply that kinetic limitations of bulk diffusion and reduction in mass accommodation coefficient may play a role in enhancing particle viscosity by suppressing condensation of semi-volatile compounds. The developed model is a useful tool for analysis and investigation of the interplay among gas-phase reactions, particle chemical composition and SOA phase state.

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