Hydroxymethanesulfonate
(HMS) in fine aerosol particles
has been
reported at significant concentrations along with sulfate under extreme
cold conditions (-35 °C) in Fairbanks, Alaska, a high latitude
city. HMS, a component of S(IV) and an adduct of formaldehyde and
sulfur dioxide, forms in liquid water. Previous studies may have overestimated
HMS concentrations by grouping it with other S(IV) species. In this
work, we further investigate HMS and the speciation of S(IV) through
the Alaskan Layered Pollution and Chemical Analysis (ALPACA) intensive
study in Fairbanks. We developed a method utilizing hydrogen peroxide
to isolate HMS and found that approximately 50% of S(IV) is HMS for
total suspended particulates and 70% for PM2.5. The remaining
unidentified S(IV) species are closely linked to HMS during cold polluted
periods, showing strong increases in concentration relative to sulfate
with decreasing temperature, a weak dependence on particle water,
and similar particle size distributions, suggesting a common aqueous
formation process. A portion of the unidentified S(IV) may originate
from additional aldehyde-S(IV) adducts that are unstable in the water-based
chemical analysis process, but further chemical characterization is
needed. These results show the importance of organic S(IV) species
in extreme cold environments that promote unique aqueous chemistry
in supercooled liquid particles.