Recent laboratory observations have shown that particle acidity increases secondary
organic aerosol (SOA) yields. However, these studies have mainly focused on biogenic …

In this study we investigate the hypothesis that oxidants present within atmospheric particles
can promote the formation of highly oxidized organic aerosol (OA) via oxidation reactions in …

A key mechanism for atmospheric secondary organic aerosol (SOA) formation occurs when
oxidation products of volatile organic compounds condense onto pre-existing particles …

The formation of secondary organic aerosol (SOA) following the ozonolysis of terpene has
been investigated intensively in recent years. The enhancement of SOA yields from the acid …

Atmospheric models of secondary organic aerosol (SOA) typically assume organic species
form a well-mixed phase. As a result, partitioning of semivolatile oxidation products into the …

Recent work has shown that particle-phase reactions contribute to the formation of
secondary organic aerosol (SOA), with enhancements of SOA yields in the presence of …

The organic component is the most abundant fraction of atmospheric submicron particles,
while the formation mechanisms of secondary organic aerosol (SOA) are not fully …

The formation of secondary organic aerosol (SOA) has been widely studied in the presence
of dry seed particles at low relative humidity (RH). At higher RH, initially dry seed particles …

Secondary organic aerosol (SOA) produced from atmospheric oxidation of organic vapors
comprises a large portion of ambient particulate matter. Currently, SOA models typically …

Photochemical oxidations of acetone were studied under different inorganic seed (NaCl,(NH
4) 2 SO 4 and NaNO 3) conditions in a self-made chamber. The results show that no …