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 …

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

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

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 …

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

Secondary organic aerosol (SOA) is a complex mixture of hundreds of semi-volatile to
extremely low-volatility organic compounds that are chemically processed in the …

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

The heterogeneous oxidation of laboratory Secondary Organic Aerosol (SOA) particles by
OH radicals was investigated. SOA particles, produced by reaction of α-pinene and O 3 …

Peroxide-containing highly oxygenated molecules (HOMs) are formed upon ozonolysis of
terpenes emitted from the biosphere and are expected to be a major driving force for the …

Aromatic hydrocarbons (ArHCs) and oxygenated aromatic hydrocarbons (ArHC–OHs) are
emitted from a variety of anthropogenic activities and are important precursors of secondary …