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

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

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) are a major contributor to fine particulate mass and wield
substantial influences on the Earth's climate and human health. Despite extensive research …

Mass accommodation is an essential process for gas–particle partitioning of organic
compounds in secondary organic aerosols (SOA). The mass accommodation coefficient is …

The kinetics of heterogeneous reactions involving supercooled organic droplets is reported
for the first time. Reactions between ozone and internally-mixed sub-micrometre particles …

The formation and aging of organic aerosols (OA) proceed through multiple steps of
chemical reaction and mass transport in the gas and particle phases, which is challenging …

The formation, atmospheric evolution, properties, and removal of organic particulate matter
remain some of the least understood aspects of atmospheric chemistry despite the …

Atmospheric aerosols exert a substantial influence on climate, ecosystems, visibility, and
human health. Although secondary organic aerosols (SOA) dominate fine-particle mass …