We compare the oxidation state and molecular composition of α‐pinene‐derived secondary
organic aerosol (SOA) by varying the types and surface areas of inorganic seed aerosol that …

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 chemical composition of secondary organic aerosol (SOA) particles, formed by the dark
ozonolysis of α-pinene, was characterized by a high-resolution time-of-flight aerosol mass …

The formation of secondary organic aerosol (SOA) from both ozonolysis and hydroxyl radical
(OH)-initiated oxidation of α-pinene under conditions of high nitric oxide (NO) concentrations …

Gas-particle partitioning theory is widely used in atmospheric models to predict organic
aerosol loadings. This theory predicts that secondary organic aerosol (SOA) yield of an …

Secondary organic aerosols (SOAs) originating from the oxidation of biogenic volatile
organic compounds such as monoterpenes by atmospheric oxidants (eg OH, ozone, and …

Despite a number of smog chamber studies of the α‐pinene/O3 system, the effect of
temperature on α‐pinene secondary organic aerosol (SOA) mass fractions (or yields) …

Secondary organic aerosol (SOA) plays a central role in air pollution and climate. However,
the description of the sources and mechanisms leading to SOA is elusive despite decades of …

It is well known that light absorption from dust and black carbon aerosols has a warming
effect on climate while light scattering from sulfate, nitrate, and sea salt aerosols has a …

The formation of secondary organic aerosol (SOA) from α-pinene ozonolysis has been
widely studied, with a recent focus on contributions from highly oxidized multifunctional …