Most chemical transport models assume instantaneous equilibrium to represent gas-particle
partitioning of semivolatile organic aerosol. This approach has been challenged by recent …

Particle phase state is a property of atmospheric aerosols that has important implications for
the formation, evolution, and gas/particle partitioning of secondary organic aerosol (SOA). In …

There are large uncertainties in the parameters dictating the gas-particle partitioning of
secondary organic aerosols (SOA), although this process has major influences on their …

This paper discusses the reversibility of gas‐particle partitioning in secondary organic
aerosol (SOA) formed from α‐pinene ozonolysis in a smog chamber. Previously, phase …

Field measurements of secondary organic aerosol (SOA) find significantly higher mass
loads than predicted by models, sparking intense effort focused on finding additional SOA …

Secondary organic aerosols (SOA) account for a substantial fraction of air particulate matter,
and SOA formation is often modeled assuming rapid establishment of gas–particle …

The partitioning of low-and semi-volatile organic compounds into and out of particles
significantly influences secondary organic aerosol formation and evolution. Most …

Secondary organic aerosols (SOA) forms a major fraction of organic aerosols in the
atmosphere. Knowledge of SOA properties that affect their dynamics in the atmosphere is …

Organic aerosol is the largest fraction of the atmospheric nonrefractory aerosol mass and
has a significant impact on climate, visibility, and human health. A significant portion of …

Secondary organic aerosol (SOA) formed from partitioning of oxidation products of
anthropogenic and biogenic volatile organic compounds (VOCs) accounts for a substantial …