The
study of aerosol particles composed of mixtures of organic
and inorganic compounds provides insights for understanding chemistry
in the atmosphere as well as information about phase transitions of
systems under confinement. In the submicron size regime, we have previously
found that liquid–liquid phase separation can be inhibited
at sufficiently small particle diameters leading to phase separated
particles at larger sizes and homogeneous particles below a threshold
diameter. In this paper, we have investigated the influence of cations
and anions in the inorganic compound (NH4
+,
Na+, SO4
2–, HSO4
–, and Cl–) on the phase separation
of submicron aerosol particles. Each of five salts were studied with
two different organic compounds. Surprisingly, a strong dependence
on the identity of the cation is evident in the size dependence of
the particle morphology, and no dependence on the anion was found.
Sodium containing samples exhibit phase separation in particles below
20 nm in diameter, whereas ammonium containing samples cease to undergo
phase separation in particles between 45 and 65 nm in diameter. The
separation relative humidity for supermicron droplets also depends
on the identity of the cation in the inorganic component if the anion
is the same across the salts compared. In addition, the correlation
between the separation relative humidity and size dependence was investigated
and displays a trend but is not a dominant feature of the data. We
explain the results in terms of hard and soft ions, where the harder
cation (Na+) leads to phase separation down to smaller
sizes while the softer cation (NH4
+) prevents
phase separation and causes particles up to a larger diameter to remain
homogeneous. This study has implications for atmospheric chemistry
in regions dominated by sea spray aerosol, which contains sodium as
the primary cation, when compared to continental aerosol, where ammonium
is an abundant cation. Additionally, these findings can be used to
understand the influence of cations on the phase transitions of confined
materials.