Water vapor uptake to particles could potentially affect organic‐aerosol mass in three ways:
first, water in the organic phase could reduce organic (equilibrium) partial pressures …

The effect of relative humidity (RH) on aerosol formation by the semi-volatile oxidation
products of the α-pinene/O3 system has been comprehensively studied. Experiments were …

This paper discusses the reversibility of gas‐particle partitioning in secondary organic
aerosol (SOA) formed from α‐pinene ozonolysis in a smog chamber. Previously, phase …

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 …

We compare the oxidation state and molecular composition of α‐pinene‐derived secondary
organic aerosol (SOA) by varying the types and surface areas of inorganic seed aerosol that …

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 …

The reactive uptake of α-pinene oxide (αPO) to acidic sulfate aerosol was studied under
humid conditions in order to gain insight into the effects of liquid–liquid phase separation on …

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

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

Secondary organic aerosols (SOA) are a major contributor to fine particulate mass and wield
substantial influences on the Earth's climate and human health. Despite extensive research …