Biogenic volatile organic compounds (VOCs) are a significant source of global secondary
organic aerosol (SOA); however, quantifying their aerosol forming potential remains a …

Laboratory chamber data serve as the basis for constraining models of secondary organic
aerosol (SOA) formation. Current models fall into three categories: empirical two-product …

Secondary organic aerosol (SOA) is an important constituent of the atmosphere where SOA
particles are formed chiefly by the condensation or reactive uptake of oxidation products of …

Secondary organic aerosol formation from volatile precursors can be thought of as a
succession of generations of reaction products. Here, we constrain first-generation SOA …

A model mechanism to describe the oxidation of α‐pinene and β‐pinene has been
developed based on the chemistry of lower alkenes and smog chamber studies of gas and …

Measurements of particle formation following the gas phase oxidation of volatile organic
compounds (VOCs) emitted by Scots pine (Pinus sylvestris L.) seedlings are reported …

2-Methyl-3-buten-2-ol (MBO) is an important biogenic volatile organic compound (BVOC)
emitted by pine trees and a potential precursor of atmospheric secondary organic aerosol …

The fraction of gasoline direct-injection (GDI) vehicles comprising the total vehicle pool is
projected to increase in the future. However, thorough knowledge about the influence of GDI …

Highly oxygenated molecules (HOMs) from the atmospheric oxidation of biogenic volatile
organic compounds are important contributors to secondary organic aerosol (SOA). Organic …

BOREAM, a detailed model for the gas-phase oxidation of α-pinene and its subsequent
formation of Secondary Organic Aerosol (SOA), is tested against a large set of SOA yield …