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) produced from atmospheric oxidation of organic vapors
comprises a large portion of ambient particulate matter. Currently, SOA models typically …

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) …

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

Formation of secondary organic aerosol (SOA) is initiated by the oxidation of volatile organic
compounds (VOCs) in the gas phase whose products subsequently partition to the particle …

Gas-particle partitioning theory is widely used in atmospheric models to predict organic
aerosol loadings. This theory predicts that secondary organic aerosol (SOA) yield of an …

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 …

Secondary organic aerosol (SOA) constitutes a significant fraction of total atmospheric
particulate loading, but there is evidence that SOA yields based on laboratory studies may …

The formation of secondary organic aerosol (SOA) following the ozonolysis of terpene has
been investigated intensively in recent years. The enhancement of SOA yields from the acid …

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