2005
DOI: 10.1029/2005gl023637
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Secondary organic aerosol formation from isoprene photooxidation under high‐NOx conditions

Abstract: The oxidation of isoprene (2‐methyl‐1,3‐butadiene) is known to play a central role in the photochemistry of the troposphere, but is generally not considered to lead to the formation of secondary organic aerosol (SOA), due to the relatively high volatility of known reaction products. However, in the chamber studies described here, we measure SOA production from isoprene photooxidation under high‐NOx conditions, at significantly lower isoprene concentrations than had been observed previously. Mass yields are low… Show more

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Cited by 332 publications
(412 citation statements)
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“…Isoprene is also known to have a small but significant yield of SOA mass formation. Depending on seed aerosol, initial precursor concentration and relative NO x levels, SOA yields in the range of 1-5 % were reported in the literature (Kroll et al, 2005;Dommen et al, 2006;Kroll et al, 2006;Dommen et al, 2009). Including SOA from isoprene in calculations of the global SOA burden increases SOA by factors between 0.5 and 2 depending on scenarios used (Henze and Seinfeld, 2006).…”
Section: Resultsmentioning
confidence: 99%
“…Isoprene is also known to have a small but significant yield of SOA mass formation. Depending on seed aerosol, initial precursor concentration and relative NO x levels, SOA yields in the range of 1-5 % were reported in the literature (Kroll et al, 2005;Dommen et al, 2006;Kroll et al, 2006;Dommen et al, 2009). Including SOA from isoprene in calculations of the global SOA burden increases SOA by factors between 0.5 and 2 depending on scenarios used (Henze and Seinfeld, 2006).…”
Section: Resultsmentioning
confidence: 99%
“…Gly may be associated with pollution sources whereas MeGly may be involved with biogenic sources such as isoprene. These α-dicarbonyls may serve as the precursors to produce secondary organic aerosols through heterogeneous reactions (Kroll et al, 2005;Liggio et al, 2005). Interestingly, levels of α-dicarbonyls in the Mangshan samples (3.5 to 271 ng m -3 , av.…”
Section: α-Dicarbonylsmentioning
confidence: 99%
“…10 Finally, the oxidation of isoprene leads to US and global biogenic SOA formation of 50% and 58%, respectively. 11,12,13 The addition of OH to isoprene results in four distinct hydroxyl alkyl isomers (Figure 1), each of which ultimately leads to different first-generation end products. Although there has been no direct experimental determination of the branching between channels, theoretical work has predicted branching of 0.67, 0.02, 0.02, and 0.29, respectively, for isomers I, II, III, and IV, 14 with an overall rate of (1.0 ( 0.1) × 10 -10 molecule -1 cm 3 s -1 .…”
Section: Introductionmentioning
confidence: 99%