Abstract. Organosulfur compounds are found to be ubiquitous in atmospheric aerosols
– a majority of which are expected to be organosulfates (OSs). Given the
atmospheric abundance of OSs, and their potential to form a variety of
reaction products upon aging, it is imperative to study the transformation
kinetics and chemistry of OSs to better elucidate their atmospheric fates
and impacts. In this work, we investigated the chemical transformation of an
α-pinene-derived organosulfate (C10H17O5SNa, αpOS-249) through heterogeneous OH oxidation at a relative humidity of 50 % in an oxidation flow reactor (OFR). The aerosol-phase reaction products
were characterized using high-performance liquid
chromatography–electrospray ionization–high-resolution mass spectrometry and ion chromatography. By monitoring the decay rates of αpOS-249,
the effective heterogeneous OH reaction rate was measured to be (6.72±0.55)×10-13 cm3 molecule−1 s−1. This
infers an atmospheric lifetime of about 2 weeks at an average OH
concentration of 1.5×106 molecules cm−3. Product
analysis shows that OH oxidation of αpOS-249 can yield more
oxygenated OSs with a nominal mass-to-charge ratio (m/z) at 247
(C10H15O5S−), 263 (C10H15O6S−), 265
(C10H17O6S−), 277 (C10H13O7S−), 279
(C10H15O7S−), and 281 (C10H17O7S−). The formation of fragmentation products,
including both small OSs (C <10) and inorganic sulfates, is found
to be insignificant. These observations suggest that functionalization
reactions are likely the dominant processes and that multigenerational
oxidation possibly leads to formation of products with one or two hydroxyl
and carbonyl functional groups adding to αpOS-249. Furthermore, all
product ions except m/z=277 have been detected in laboratory-generated
α-pinene-derived secondary organic aerosols as well as in
atmospheric aerosols. Our results reveal that OSs freshly formed from the
photochemical oxidation of α-pinene could react further to form OSs
commonly detected in atmospheric aerosols through heterogeneous OH
oxidation. Overall, this study provides more insights into the sources,
transformation, and fate of atmospheric OSs.