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From:Atmospheric Chemistry and Physics (Vol. 22, Issue 9) Peer-ReviewedReaction with ozone is an important atmospheric removal process for alkenes. The ozonolysis reaction produces carbonyls and carbonyl oxides (Criegee intermediates, CI), which can rapidly decompose to yield a range of...
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From:Atmospheric Chemistry and Physics (Vol. 21, Issue 13) Peer-ReviewedSecondary organic aerosols (SOA) are major components of atmospheric fine particulate matter, affecting climate and air quality. Mounting evidence exists that SOA can adopt glassy and viscous semisolid states, impacting...
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From:Atmospheric Chemistry and Physics (Vol. 18, Issue 13) Peer-Reviewed
Reaction with the hydroxyl (OH) radical is the dominant removal process for volatile organic compounds (VOCs) in the atmosphere. Rate coefficients for reactions of OH with VOCs are therefore...
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From:Atmospheric Chemistry and Physics (Vol. 18, Issue 18) Peer-Reviewed
Atmospheric chambers have been widely used to study secondary organic aerosol (SOA) properties and formation from various precursors under different controlled environmental conditions and to develop parameterization...
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From:Atmospheric Chemistry and Physics (Vol. 19, Issue 11) Peer-Reviewed
Organic peroxy radicals (RO.sub.2 ), formed from the degradation of hydrocarbons and other volatile organic compounds (VOCs), play a key role in tropospheric oxidation mechanisms. Several competing reactions may be...
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From:Atmospheric Chemistry and Physics (Vol. 20, Issue 21) Peer-ReviewedReaction with ozone (O.sub.3) is an important removal process for unsaturated volatile organic compounds (VOCs) in the atmosphere. Rate coefficients for reactions of O.sub.3 with VOCs are therefore essential parameters...
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From:Atmospheric Chemistry and Physics (Vol. 18, Issue 13) Peer-Reviewed
Reaction with the hydroxyl (OH) radical is the dominant removal process for volatile organic compounds (VOCs) in the atmosphere. Rate coefficients for the reactions of OH with VOCs are therefore essential parameters...