Secondary organic aerosol (SOA) consists of compounds with a wide range of volatilities
and its ambient concentration is sensitive to this volatility distribution. Recent field studies …

Peroxide-containing highly oxygenated molecules (HOMs) are formed upon ozonolysis of
terpenes emitted from the biosphere and are expected to be a major driving force for the …

Biomass burning is the largest combustion-related source of volatile organic compounds
(VOCs) to the atmosphere. We describe the development of a state-of-the-science model to …

While the role of highly oxygenated molecules (HOMs) in new particle formation (NPF) and
secondary organic aerosol (SOA) formation is not in dispute, the interplay between HOM …

Secondary organic aerosol (SOA) formation from mixtures of volatile precursors may be
influenced by the molecular interactions of the components of the mixture. Here, we report …

Previous laboratory and field studies suggest that oxidation of organic aerosols can be a
source of oxygenated volatile organic compounds (OVOC). Using measurements of …

This study examined the formation and growth of secondary organic aerosols (SOA)
generated when ozone was added to a 1m3 glass chamber that contained either pine …

Aerosols produced from the oxidation of volatile/semi-volatile organic compounds
(VOCs/SVOCs), known as secondary organic aerosol (SOA), account for a significant …

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

SOA formation from benzene, toluene, m-xylene, and their corresponding phenolic
compounds were investigated using the UCR/CE-CERT Environmental Chamber to …