Atmospheric oxidation of sulfur dioxide
(SO2) forms
sulfate-containing aerosol particles that impact air quality, climate,
and human and ecosystem health. It is well-known that in-cloud oxidation
of SO2 frequently dominates over gas-phase oxidation on
regional and global scales. Multiphase oxidation involving aerosol
particles, fog, and cloud droplets has been generally thought to scale
with liquid water content (LWC) so multiphase oxidation would be negligible
for aerosol particles due to their low aerosol LWC. However, recent
field evidence, particularly from East Asia, shows that fast sulfate
formation prevails in cloud-free environments that are characterized
by high aerosol loadings. By assuming that the kinetics of cloud water
chemistry prevails for aerosol particles, most atmospheric models
do not capture this phenomenon. Therefore, the field of aerosol SO2 multiphase chemistry has blossomed in the past decade, with
many oxidation processes proposed to bridge the difference between
modeled and observed sulfate mass loadings. This review summarizes
recent advances in the fundamental understanding of the aerosol multiphase
oxidation of SO2, with a focus on environmental conditions
that affect the oxidation rate, experimental challenges, mechanisms
and kinetics results for individual reaction pathways, and future
research directions. Compared to dilute cloud water conditions, this
paper highlights the differences that arise at the molecular level
with the extremely high solute strengths present in aerosol particles.