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 …

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

The prevailing treatment of secondary organic aerosol formation in atmospheric models is
based on the assumption of instantaneous gas–particle equilibrium for the condensing …

Evidence has accumulated that secondary organic aerosols (SOAs) exhibit complex
morphologies with multiple phases that can adopt amorphous semisolid or glassy phase …

When simulating the formation and life cycle of secondary organic aerosol (SOA) with
chemical transport models, it is often assumed that organic molecules are well mixed within …

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

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

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

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

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