Organic peroxides (POs) are organic molecules with one or more peroxide (− O–O−)
functional groups. POs are commonly regarded as chemically labile termination products …

Environmental chambers have been playing a vital role in atmospheric chemistry research
for seven decades. In last decade, oxidation flow reactors (OFR) have emerged as a …

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 …

Abstract Organic peroxy radicals (RO 2), formed from the degradation of hydrocarbons and
other volatile organic compounds (VOCs), play a key role in tropospheric oxidation …

Organic peroxy radicals (RO 2) and Criegee intermediates (CI, carbonyl oxides) are key
reactive species in atmospheric chemistry, and can proceed various reactions influencing …

The least volatile organic compounds participating in atmospheric new-particle formation
are very likely accretion products from self-and cross-reactions of peroxy radicals (RO 2). It …

Chlorine-initiated oxidation of alkanes has been shown to rapidly form secondary organic
aerosol (SOA) at higher yields than OH–alkane reactions. However, the effects of alkane …

Oxidation flow reactors (OFRs) are a promising complement to environmental chambers for
investigating atmospheric oxidation processes and secondary aerosol formation. However …

The reaction of peroxy radicals, RO 2, with OH radicals has long been ignored to play any
role in atmospheric chemistry. Recent experimental and modeling studies show however …

Formic and acetic acid concentrations are particularly high over forested areas of the world.
However, the gas-phase mechanisms for producing these acids are poorly understood even …