Functionalization vs. fragmentation: n-aldehyde oxidation mechanisms and secondary organic aerosol formation.
Because of their relatively well-understood chemistry and atmospheric relevance, aldehydes represent a good model system for carbon-carbon fragmentation reactions in organic-aerosol aging mechanisms. Small aldehydes such as ethanal and propanal react with OH radicals under high NO(x) conditions to form formaldehyde and ethanal, respectively, with nearly unit yield. CO(2) is formed as a coproduct. This path implies the formation of the C(n-1) aldehyde, or an aldehyde with one fewer methylene group than the parent. However, as the carbon number of the n-aldehyde increases, reaction with the carbon backbone becomes more likely and the C(n-1) formation path becomes less important. In this work we oxidized n-pentanal, n-octanal, n-undecanal and n-tridecanal with OH radicals at high NO(x). The C(n-1) aldehyde molar yields after the peroxyl radical + NO reaction were 69 ± 15, 36 ± 10, 16 ± 5 and 4 ± 1%, respectively. Complementary structure-activity relationship calculations of important rate constants enable estimates of branching ratios between several intermediates of the C(n)n-aldehyde reaction with OH: C(n) peroxyacyl nitrate versus C(n) alkoxyacyl radical formation, C(n-1) alkyl nitrate versus C(n-1) alkoxy radical, and C(n-1) aldehyde formation versus isomerization products. We also measured SOA mass yields, which we compare with analogous n-alkanes to understand the effect of fragmentation on organic-aerosol formation.
Chacon-Madrid
Heber J
HJ
Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, USA.
Presto
Albert A
AA
Donahue
Neil M
NM
D000336:Aerosols; D000447:Aldehydes / Q000737:chemistry*; D017665:Hydroxyl Radical / Q000737:chemistry; D009569:Nitric Oxide / Q000737:chemistry; D010084:Oxidation-Reduction
D000336:Aerosols; D000447:Aldehydes; D009569:Nitric Oxide; D017665:Hydroxyl Radical