Preprints
https://doi.org/10.5194/egusphere-2024-1690
https://doi.org/10.5194/egusphere-2024-1690
05 Jul 2024
 | 05 Jul 2024

The role of interfacial tension in the size-dependent phase separation of atmospheric aerosol particles

Ryan Schmedding and Andreas Zuend

Abstract. Atmospheric aerosol particles span orders of magnitude in size. In ultrafine particles, the energetic contributions of surfaces and interfaces to the Gibbs energy become significant and increase in importance as particle diameter decreases. For these particles, the thermodynamic equilibrium state depends on size, composition, and temperature. Various aerosol systems have been observed to undergo liquid–liquid phase separation (LLPS), impacting equilibrium gas–particle partitioning, modifying physicochemical properties of the particle phases, and influencing cloud droplet activation. Numerous laboratory experiments have characterized the onset relative humidity of LLPS in larger aerosol particles and macroscopic bulk systems. However, in sufficiently small particles, the interfacial tension between two liquid phases constitutes an energetic barrier that may prevent the formation of an additional liquid phase. Determining said small-size limit is a key question.

We introduce a predictive droplet model based on the Aerosol Inorganic–Organic Mixtures Functional groups Activity Coefficients model. This model enables size-dependent computations of surface and interfacial tension effects on bulk–surface partitioning within phase-separated and single-phase particles. We evaluate four approaches for computing interfacial tension in multicomponent droplets, including a new method introduced in this work. Of the approaches tested, Antonov's rule best matches observed liquid–liquid interfacial tensions in highly immiscible mixtures, while a modified Butler equation fits well in more miscible systems. We find that two approaches substantially lower the onset relative humidity of LLPS for the studied systems.

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Ryan Schmedding and Andreas Zuend

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • CC1: 'Comment on egusphere-2024-1690', Alison Bain, 09 Jul 2024
  • RC1: 'Comment on egusphere-2024-1690', Anonymous Referee #1, 29 Jul 2024
    • AC2: 'Reply on RC1', Ryan Schmedding, 19 Sep 2024
    • AC4: 'Reply on RC1', Ryan Schmedding, 18 Oct 2024
  • RC2: 'Comment on egusphere-2024-1690', Anonymous Referee #2, 18 Sep 2024
    • AC3: 'Reply on RC2', Ryan Schmedding, 19 Sep 2024

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • CC1: 'Comment on egusphere-2024-1690', Alison Bain, 09 Jul 2024
  • RC1: 'Comment on egusphere-2024-1690', Anonymous Referee #1, 29 Jul 2024
    • AC2: 'Reply on RC1', Ryan Schmedding, 19 Sep 2024
    • AC4: 'Reply on RC1', Ryan Schmedding, 18 Oct 2024
  • RC2: 'Comment on egusphere-2024-1690', Anonymous Referee #2, 18 Sep 2024
    • AC3: 'Reply on RC2', Ryan Schmedding, 19 Sep 2024
Ryan Schmedding and Andreas Zuend
Ryan Schmedding and Andreas Zuend

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Short summary
Four different approaches for computing the interfacial tension between liquid phases in aerosol particles were tested for particles with diameters from 10 nm to more than 5 μm. Antonov's rule led to the strongest reductions in the onset relative humidity of liquid–liquid phase separation and reproduced measured interfacial tensions for highly immiscible systems. A modified form of the Butler equation was able to best reproduce measured interfacial tensions in more miscible systems.