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 …

We present measurements of the isothermal evaporation of α-pinene ozonolysis secondary
organic aerosol (SOA). Using a novel, filter-based method, we reproduce literature …

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 …

Secondary organic aerosols (SOA) dominate atmospheric organic aerosols that affect
climate, air quality, and health. Recent studies indicate that, contrary to previously held …

The volatility of oxidation products of volatile organic compounds (VOCs) in the atmosphere
is a key factor to determine if they partition into the particle phase contributing to secondary …

The thermally induced evaporation of secondary organic aerosol (SOA) has been
characterized for SOA formed from the dark ozonolysis of α-pinene at initial mass …

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

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 …

Secondary Organic Aerosol (SOA) affects atmospheric composition, air quality and radiative
transfer, however major difficulties are encountered in the development of reliable models …

Chemical composition, size distributions, and degree of oligomerization of secondary
organic aerosol (SOA) from α-pinene (C 10 H 16) ozonolysis were investigated for low …