Hydroxymethanesulfonate (CH2(OH)SO3
–, HMS) has been found to be an important organosulfur
compound in
atmospheric aerosols. However, its atmospheric fate is largely uncertain.
In this work, we investigated the heterogeneous OH oxidation of HMS
using an oxidation flow reactor. In particular, we examined the rate
and chemistry of the sulfur conversion from its organic form to its
inorganic counterparts upon oxidation by quantifying HMS and inorganic
sulfur species (i.e., sulfate (SO4
2–)
and peroxydisulfate (S2O8
2–) ions) by using ion chromatography. Kinetic data show that OH oxidation
of HMS can proceed efficiently with an effective OH uptake coefficient,
γ
eff
of 0.35 ± 0.03. Upon oxidation,
the formation of SO4
2– and S2O8
2– can explain the aerosol sulfur
conversion. An aerosol sulfur mass closure was also obtained by quantifying
the amount of HMS, SO4
2–, and S2O8
2– before and after oxidation. Kinetic
model simulations show that reaction kinetics and product formation
can be well explained by a series of aerosol-phase chain reactions
initiated by the sulfite radical anion (SO3
•–) under our experimental conditions. Overall, our results highlight
a significant conversion of organic sulfur from HMS to inorganic sulfur
species, including S2O8
2– upon
heterogeneous OH oxidation.