Secondary organic aerosol formation from limonene ozonolysis: homogeneous and heterogeneous influences as a function of NO(x).
Limonene has a high emission rate both from biogenic sources and from household solvents. Here we examine the limonene + ozone reaction as a source for secondary organic aerosol (SOA). Our data show that limonene has very high potential to form SOA and that NO(x) levels, O(3) levels, and UV radiation all influence SOA formation. High SOA formation is observed under conditions where both double bonds in limonene are oxidized, but those conditions depend strongly on NO(x). At low NO(x), heterogeneous oxidation of the terminal double bond follows the initial limonene ozonolysis (at the endocyclic double bond) almost immediately, making the initial reaction rate limiting. This requires a high uptake coefficient between ozone and the first-generation, unsaturated organic particles. However, at high NO(x), this heterogeneous processing is inhibited and gas-phase oxidation of the terminal double bond dominates. Although this chemistry is slower, it also yields products with low volatility. UV light suppresses production of the lowest volatility products, as we have shown in earlier studies of the alpha-pinene + ozone reaction.
Zhang
Jieyuan
J
Center for Atmospheric Particle Studies, Carnegie Mellon University, Pittsburgh, Pennsylvania 15213, USA.
Huff Hartz
Kara E
KE
Pandis
Spyros N
SN
Donahue
Neil M
NM
D000336:Aerosols; D053138:Cyclohexenes / Q000737:chemistry*; D000077222:Limonene; D013058:Mass Spectrometry; D015394:Molecular Structure; D009589:Nitrogen Oxides / Q000737:chemistry*; D010126:Ozone / Q000737:chemistry*; D013729:Terpenes / Q000737:chemistry*; D014466:Ultraviolet Rays; D014867:Water / Q000737:chemistry
D000336:Aerosols; D053138:Cyclohexenes; D009589:Nitrogen Oxides; D013729:Terpenes; D014867:Water; D010126:Ozone; D000077222:Limonene