In the presence of inorganic salts,
secondary organic aerosol (SOA)
undergoes liquid–liquid phase separation (LLPS), liquid–solid
phase separation, or a homogeneous phase in ambient air. In this study,
a regression model was derived to predict aerosol phase separation
relative humidity (SRH) for various organic and inorganic mixes. The
model implemented organic physicochemical parameters (i.e., oxygen
to carbon ratio, molecular weight, and hydrogen-bonding ability) and
the parameters related to inorganic compositions (i.e., ammonium,
sulfate, nitrate, and water). The aerosol phase data were observed
using an optical microscope and also collected from the literature.
The crystallization of aerosols at the effloresce RH (ERH) was semiempirically
predicted with a neural network model. Overall, the greater SRH appeared
for the organic compounds with the lower oxygen to carbon ratios or
the greater molecular weight and the higher aerosol acidity or the
larger fraction of inorganic nitrate led to the lower SRH. The resulting
model has been demonstrated for three different chamber-generated
SOA (originated from β-pinene, toluene, and 1,3,5-trimethylbenzene),
which were internally mixed with the inorganic aqueous system of ammonium–sulfate–water.
For all three SOA systems, both observations and model predictions
showed LLPS at RH <80%. In the urban atmosphere, LLPS is likely
a frequent occurrence for the typical anthropogenic SOA, which originates
from aromatic and alkane hydrocarbon.