Secondary organic aerosol formation from low-NO(x) photooxidation of dodecane: evolution of multigeneration gas-phase chemistry and aerosol composition.
about
Size distribution dynamics reveal particle-phase chemistry in organic aerosol formationAtmospheric autoxidation is increasingly important in urban and suburban North America.Secondary organic aerosol formation from fossil fuel sources contribute majority of summertime organic mass at BakersfieldModeling the influence of alkane molecular structure on secondary organic aerosol formationChemical Mechanisms of Aging of Aerosol Formed from the Reaction of n-Pentadecane with OH Radicals in the Presence of NOxSimilarities in STXM-NEXAFS Spectra of Atmospheric Particles and Secondary Organic Aerosol Generated from Glyoxal, α-Pinene, Isoprene, 1,2,4-Trimethylbenzene, and d-Limonene
P2860
Secondary organic aerosol formation from low-NO(x) photooxidation of dodecane: evolution of multigeneration gas-phase chemistry and aerosol composition.
description
2012 nî lūn-bûn
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2012年の論文
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2012年学术文章
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2012年学术文章
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2012年学术文章
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name
Secondary organic aerosol formation from low-NO
@nl
Secondary organic aerosol form ...... istry and aerosol composition.
@en
type
label
Secondary organic aerosol formation from low-NO
@nl
Secondary organic aerosol form ...... istry and aerosol composition.
@en
prefLabel
Secondary organic aerosol formation from low-NO
@nl
Secondary organic aerosol form ...... istry and aerosol composition.
@en
P2093
P356
P1476
Secondary organic aerosol form ...... istry and aerosol composition.
@en
P2093
Christine L Loza
Jill S Craven
John H Seinfeld
Katherine A Schilling
Lindsay D Yee
Manjula R Canagaratna
Nga Lee Ng
Paul J Ziemann
Richard C Flagan
P304
P356
10.1021/JP211531H
P407
P577
2012-04-10T00:00:00Z