A key mechanism for atmospheric secondary organic aerosol (SOA) formation occurs when
oxidation products of volatile organic compounds condense onto pre-existing particles …

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 …

Recent laboratory observations have shown that particle acidity increases secondary
organic aerosol (SOA) yields. However, these studies have mainly focused on biogenic …

In this study we investigate the hypothesis that oxidants present within atmospheric particles
can promote the formation of highly oxidized organic aerosol (OA) via oxidation reactions in …

The formation of secondary organic aerosol (SOA) has been widely studied in the presence
of dry seed particles at low relative humidity (RH). At higher RH, initially dry seed particles …

Secondary organic aerosols (SOAs) affect human health and climate change prediction;
however, the factors (eg, temperature, acidity of pre-existing particles, and oxidants) …

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

Secondary organic aerosol (SOA) is a complex mixture of hundreds of semi-volatile to
extremely low-volatility organic compounds that are chemically processed in the …

Semi‐empirical secondary organic aerosol (SOA) models typically assume a well‐mixed
organic aerosol phase even in the presence of hydrophobic primary organic aerosols (POA) …

Recent work has shown that particle-phase reactions contribute to the formation of
secondary organic aerosol (SOA), with enhancements of SOA yields in the presence of …