Hydrocarbons are emitted into the Earth's atmosphere in very large quantities by human and biogenic activities. Their atmospheric oxidation processes almost exclusively yield RO2 radicals as reactive intermediates whose atmospheric fate is not yet fully unraveled. Herein, we show that gas-phase reactions of two RO2 radicals produce accretion products composed of the carbon backbone of both reactants. The rates for accretion product formation are very high for RO2 radicals bearing functional groups, competing with those of the corresponding reactions with NO and HO2. This pathway, which has not yet been considered in the modelling of atmospheric processes, can be important, or even dominant, for the fate of RO2 radicals in all areas of the a...
Oxidation flow reactors (OFRs) are a promising complement to environmental chambers for investigati...
Explaining the formation of secondary organic aerosol is an intriguing question in atmospheric scien...
Isoprene, C5H8, inserts about half of the non-methane carbon flux of biogenic origin into the atmosp...
Hydrocarbons are emitted into the Earth's atmosphere in very large quantities by human and biogenic ...
The formation of accretion products ("dimers") from recombination reactions of peroxyl radicals (RO2...
Organic peroxy radicals (RO2) play a pivotal role in the degradation of hydrocarbons. The autoxidati...
The recombination ("dimerization") of peroxyl radicals (RO2 center dot) is one of the pathways sugge...
The gas-phase mechanism of the formation of highly oxidized multifunctional organic compounds (HOMs)...
alpha-Pinene (C10H16) represents one of the most important biogenic emissions in the atmosphere. Its...
Peroxy (RO2) and alkoxy (RO) radicals are prototypical intermediates in any hydrocarbon oxidation. I...
Dimeric accretion products have been observed both in atmospheric aerosol particles and in the gas p...
Organic peroxy radicals (RO2), formed from the degradation of hydrocarbons and other volatile organi...
We evaluate monoterpene-derived peroxy radical (MT-RO2) unimolecular autoxidation and self- and cros...
Atmospheric autoxidation of volatile organic compounds (VOC) leads to prompt formation of highly oxi...
α-Pinene (C10H16) represents one of the most important biogenic emissions in the atmosphere. Its oxi...
Oxidation flow reactors (OFRs) are a promising complement to environmental chambers for investigati...
Explaining the formation of secondary organic aerosol is an intriguing question in atmospheric scien...
Isoprene, C5H8, inserts about half of the non-methane carbon flux of biogenic origin into the atmosp...
Hydrocarbons are emitted into the Earth's atmosphere in very large quantities by human and biogenic ...
The formation of accretion products ("dimers") from recombination reactions of peroxyl radicals (RO2...
Organic peroxy radicals (RO2) play a pivotal role in the degradation of hydrocarbons. The autoxidati...
The recombination ("dimerization") of peroxyl radicals (RO2 center dot) is one of the pathways sugge...
The gas-phase mechanism of the formation of highly oxidized multifunctional organic compounds (HOMs)...
alpha-Pinene (C10H16) represents one of the most important biogenic emissions in the atmosphere. Its...
Peroxy (RO2) and alkoxy (RO) radicals are prototypical intermediates in any hydrocarbon oxidation. I...
Dimeric accretion products have been observed both in atmospheric aerosol particles and in the gas p...
Organic peroxy radicals (RO2), formed from the degradation of hydrocarbons and other volatile organi...
We evaluate monoterpene-derived peroxy radical (MT-RO2) unimolecular autoxidation and self- and cros...
Atmospheric autoxidation of volatile organic compounds (VOC) leads to prompt formation of highly oxi...
α-Pinene (C10H16) represents one of the most important biogenic emissions in the atmosphere. Its oxi...
Oxidation flow reactors (OFRs) are a promising complement to environmental chambers for investigati...
Explaining the formation of secondary organic aerosol is an intriguing question in atmospheric scien...
Isoprene, C5H8, inserts about half of the non-methane carbon flux of biogenic origin into the atmosp...