Highly oxygenated organic molecules (HOM) are formed in the atmosphere via autoxidation
involving peroxy radicals arising from volatile organic compounds (VOC). HOM condense on …

Dimethyl sulfide (DMS), emitted from the oceans, is the most abundant biological source of
sulfur to the marine atmosphere. Atmospheric DMS is oxidized to condensable products that …

Gas-phase autoxidation—regenerative peroxy radical formation following intramolecular
hydrogen shifts—is known to be important in the combustion of organic materials. The …

Secondary organic aerosol (SOA) is ubiquitous in the atmosphere and plays a pivotal role in
climate, air quality, and health. The production of low-volatility dimeric compounds through …

A large data set of rate coefficients for H migration in peroxy radicals is presented and
supplemented with literature data to derive a structure–activity relationship (SAR) for the title …

The gas-phase oxidation of organic compounds is an important chemical process in the
Earth's atmosphere. It governs oxidant levels and controls the production of key secondary …

Organic hydrotrioxides (ROOOH) are known to be strong oxidants used in organic synthesis.
Previously, it has been speculated that they are formed in the atmosphere through the gas …

The design of circular polymers has emerged as a necessity due to the lack of efficient
recycling methods for many commodity plastics, particularly those used in durable products …

Atmospheric oxidation of monoterpenes (emitted primarily by evergreen trees) is known to
contribute to the formation and growth of aerosol particles. While recent research has tied …

Emissions of aromatic compounds cause air pollution and detrimental health effects. Here,
we explore the reaction kinetics and products of key radicals in benzene photo-oxidation …