Abstract. Secondary organic aerosols (SOAs) affect human health and
climate change prediction; however, the factors (e.g., temperature, acidity
of pre-existing particles, and oxidants) influencing their formation are not
sufficiently resolved. Using a compact chamber, the temperature and acidity
dependence of SOA yields and chemical components in SOA from α-pinene ozonolysis were systematically investigated under 278, 288, and
298 K temperatures using neutral ((NH4)2SO4) and acidic
(H2SO4+((NH4)2SO4)) seed aerosols. SOA components
with m/z less than 400 were analyzed using negative electrospray ionization
liquid-chromatography time-of-flight mass spectrometry. Based on the
slightly negative temperature dependence of the SOA yields, the enthalpies
of vaporization under neutral and acidic seed conditions were estimated to
be 25 and 44 kJ mol−1, respectively. In addition, SOA yields increased
with an increase in the acidity of seed particles (solid/near-solid state)
at low SOA mass loadings, when compared with the seed particle amounts.
Acidity dependence analysis of the chemical formula, molecular mass, and O:C
ratio of the detected compounds indicated the enhanced formation of multiple
oligomers in the wide molecular mass range with a wide range of O:C ratios
under acidic seed conditions. The peak abundances of some chemical compounds
increased with an increase in the acidity of seed particles (e.g., m/z 197,
311, 313, 339, 355, and 383), while decreases in the peak abundances of some
chemical compounds were observed (e.g., m/z 171, 185, 215, 343, and 357). The
acidity dependence could be explained by acid-catalyzed heterogeneous
reactions or acid-catalyzed decomposition of hydroperoxides. In addition,
organosulfate (OS) formation was observed under acidic seed conditions. Six
out of the 11 detected OSs were potentially formed via the aldehyde +
HSO4- pathway.