Abstract
Organic molecules at the aqueous interfaces of droplets and aerosols can influence multiphase chemistry, and cloud condensation nuclei activity. While surface tension measurements on flat surfaces are commonly used to quantify organic partitioning and structure, extending these measurements to more realistic aerosols that might exist in metastable, supercooled and supersaturated states remains a challenge. Here, we use aerosol velocity map imaging X-ray photoelectron spectroscopy (A-VMI-XPS), a surface-sensitive and in-situ technique, to study the partitioning and structure of a model surfactant (n-octyl β-D-thioglucopyranoside, OTG) in submicron aqueous aerosols with a mean radius of 116 nm. After accounting for finite size effects and evaporative cooling, we find the bulk concentrations of OTG in the aerosol are depleted 1,400-fold relative to macroscopic solutions. At the low temperatures of the experiment (ca. ~188K), we obtain a Langmuir equilibrium constant of 1,300 m3 mol−1, which corresponds to 7.6 m3 mol−1 at room temperature; a value that is consistent with prior literature reports. Analysis of photoelectron angular distributions, peak areas, and secondary electron escape barriers indicates a transition from a disordered surfactant layer at low [OTG] to a more structured layer at high [OTG]. These results link macroscopic surface tension measurements to nanoparticle surfactant behavior and demonstrate the utility of A-VMI-XPS in probing surfactant coating structure on free aerosols, with implications for understanding the impact of organic coatings on cloud formation and atmospheric chemistry.
Supplementary materials
Title
Supporting Information
Description
Contents
S1. Particle Size Distributions
S2. Aerodynamic Lens Details
S3. Repeat of XPS Spectra
S4. Photoelectron Peak Assignment
S5. Photoelectron Peak Fitting Details
S6. Langmuir Fits to Macroscopic Flat Water Surface Tension Data
S7. Beta Parameter Fitting Details
S8. Secondary Electron Signal Fitting Details
S9. Experimental Data
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