Atmospheric oxidation
of volatile organic compounds, such as isoprene,
and subsequent condensation or heterogeneous reactions lead to the
formation of secondary organic aerosol (SOA), a ubiquitous component
of submicron aerosol. Liquid–liquid phase-separated organic–inorganic
aerosol particles have been observed in the laboratory and field;
however, the impacts of multiphase reactions on aerosol viscosity
are not well understood for phase-separated aerosol particles. In
this study, phase-separated aerosol particles were reacted with gaseous
isoprene epoxydiol (IEPOX), an abundant isoprene oxidation product.
Acidic sulfate particles (H2SO4 + (NH4)2SO4 at pH = 1.4) were coated with laboratory-generated
biogenic SOA (α-pinene + O3) and anthropogenic SOA
(toluene + OH), resulting in a core–shell morphology. After
reaction with IEPOX, the phase-separated aerosol particles no longer
displayed characteristics of a liquid core. Instead, they became irregularly
shaped, taller after impaction onto substrates, and had decreased
spreading ratios for both types of SOA, implying an increase in particle
viscosity. As the SOA from α-pinene and toluene was already
viscous, this is indicative of a change in phase state for the core
from liquid to viscous state. An example reaction that may be facilitating
this phase change is IEPOX reaction with inorganic sulfate to produce
organosulfates, especially after IEPOX diffuses through the organic
coating. The modification of the aerosol physicochemical properties
suggests that phase state is dynamic over the atmospheric lifetime
of SOA-containing particles, with multiphase chemistry between aerosol
particles and gaseous species leading to more viscous aerosol after
uptake of isoprene oxidation products (e.g., IEPOX).