Size Dependence of Organic/Inorganic Aerosol Morphology and the Role of Oxidation and Aromaticity of the Organic Component

Atmospheric aerosol particles can exist in a phase separated state depending on their chemical components and size as well as relative humidity and temperature conditions, although the effects of these conditions on particle morphology is not well constrained. Whether a system is phase separated or not has implications for new particle growth, cloud condensation nucleus formation, ice nucleation, and heterogeneous chemistry. In this study, the identity of the organic species in a binary organic/inorganic phase separating system was found to influence the phase separation properties of these internally mixed aerosol particles. Aerosol particles composed of a carboxylic acid, ammonium sulfate, and water were generated, dried, and characterized using transmission electron microscopy which revealed the influence of aromaticity and the oxidation of the organic component on the size dependence of phase separation. Organic oxidation was defined by the elemental oxygen to carbon ratio (O:C ratio) and lipophilicity (characterized by the negative distribution coefficient at pH 5.5, -log D5.5) for each compound. The span of particle diameters at which both phase-separated and homogeneous particles are found, or the transition region, was evaluated using a logistic regression to calculate the diameters at which there is a 20%, 50%, and 80% probability of a phase separated morphology. The seven systems containing aliphatic organic species showed a positive correlation between the particle diameters in the transition region and organic oxidation while the four systems containing aromatic organic species showed transition regions with a tentative negative correlation until phase separation was arrested. Overall, these results show how aromaticity and oxygen content of organic species can determine the morphologies of environmentally relevant aerosol particles and may provide improved constraints for particle-resolved atmospheric models.

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Work Title Size Dependence of Organic/Inorganic Aerosol Morphology and the Role of Oxidation and Aromaticity of the Organic Component
Access
Open Access
Creators
  1. Emma C. Tackman
  2. Komal Jaswal
  3. Miriam Arak Freedman
Keyword
  1. Oxidation state
  2. Octanol-water partitioning coefficient
  3. Log D
  4. Liquid-liquid phase separation
  5. Aerosol phase transitions
  6. Atmospheric aerosol particles
  7. Transmission electron microscopy
License In Copyright (Rights Reserved)
Work Type Article
Publisher
  1. ACS ES&T Air
Publication Date April 6, 2024
Publisher Identifier (DOI)
  1. https://doi.org/10.1021/acsestair.3c00099
Deposited March 31, 2025

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Version 1
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  • Created
  • Updated
  • Updated
  • Updated Publisher, Publisher Identifier (DOI), Description, and 1 more Show Changes
    Publisher
    • Environmental Science and Technology: Air
    Publisher Identifier (DOI)
    • 10.1021/acsestair.3c00099
    Description
    • Atmospheric aerosol particles can exist in a phase separated state depending on their chemical components and size as well as relative humidity and temperature conditions, although the effects of these conditions on particle morphology is not well constrained. Whether a system is phase separated or not has implications for new particle growth, cloud condensation nucleus formation, ice nucleation, and heterogeneous chemistry. In this study, the identity of the organic species in a binary organic/inorganic phase separating system was found to influence the phase separation properties of these internally mixed aerosol particles. Aerosol particles composed of a carboxylic acid, ammonium sulfate, and water were generated, dried, and characterized using transmission electron microscopy which revealed the influence of aromaticity and the oxidation of the organic component on the size dependence of phase separation. Organic oxidation was defined by the elemental oxygen to carbon ratio (O:C ratio) and lipophilicity (characterized by the negative distribution coefficient at pH 5.5, -log D5.5) for each compound. The span of particle diameters at which both phase-separated and homogeneous particles are found, or the transition region, was evaluated using a logistic regression to calculate the diameters at which there is a 20%, 50%, and 80% probability of a phase separated morphology. The seven systems containing aliphatic organic species showed a positive correlation between the particle diameters in the transition region and organic oxidation while the four systems containing aromatic organic species showed transition regions with a tentative negative correlation until phase separation was arrested. Overall, these results show how aromaticity and oxygen content of organic species can determine the morphologies of environmentally relevant aerosol particles and may provide improved constraints for particle-resolved atmospheric models.
    Publication Date
    • 2024-04-06
  • Added Creator Emma C. Tackman
  • Added Creator Komal Jaswal
  • Added Creator Miriam Freedman
  • Added OC manuscript revision draft 4.pdf
  • Added OC SI revision.pdf
  • Updated License Show Changes
    License
    • https://rightsstatements.org/page/InC/1.0/
  • Published
  • Updated
  • Updated Keyword, Publisher, Publisher Identifier (DOI) Show Changes
    Keyword
    • Oxidation state, Octanol-water partitioning coefficient, Log D, Liquid-liquid phase separation, Aerosol phase transitions, Atmospheric aerosol particles, Transmission electron microscopy
    Publisher
    • Environmental Science and Technology: Air
    • ACS ES&T Air
    Publisher Identifier (DOI)
    • 10.1021/acsestair.3c00099
    • https://doi.org/10.1021/acsestair.3c00099
  • Renamed Creator Miriam Arak Freedman Show Changes
    • Miriam Freedman
    • Miriam Arak Freedman