dynamic consideration of smog chamber experiments
Clicks: 6
ID: 230981
2017
Article Quality & Performance Metrics
Overall Quality
Not rated
Combines reader engagement with the AI quality analysis. This
article has not been analysed, so there is no overall score —
reader engagement is measured and shown alongside.
Reader Engagement
Emerging Content
1.5
/100
6 views
4 readers
AI Quality Assessment
Not analyzed
Readership in this journal
EmergingRanked #816 of 850 articles by views in Journal of agricultural and food chemistry
Most read
Least read
Bar heights use a square-root scale. Only the 120 most-read articles are drawn; the journal has 850 in total.
Mint this article as an NFT
Not yet mintedCreate a permanent, verifiable on-chain record of this article on the Scimatic Network. The NFT is held in your Journament account, and you can withdraw it to your own wallet at any time.
5
SUSD
one-off · no wallet required
Abstract
Recent studies of the α-pinene + ozone reaction that address
particle nucleation show relatively high molar yields of highly oxidized
multifunctional organic molecules with very low saturation concentrations
that can form and grow new particles on their own. However,
numerous smog-chamber experiments addressing secondary organic aerosol (SOA)
mass yields, interpreted via equilibrium partitioning theory, suggest that
the vast majority of SOA from α-pinene is semivolatile. We explore
this paradox by employing a dynamic volatility basis set (VBS) model that
reproduces the new-particle growth rates observed in the CLOUD experiment at
CERN and then modeling SOA mass yield experiments conducted at Carnegie
Mellon University (CMU). We find that the base-case simulations do
overpredict observed SOA mass but by much less than an equilibrium analysis
would suggest; this is because delayed condensation of vapors suppresses the
apparent mass yields early in the chamber experiments. We further find that a
second VBS model featuring substantial oligomerization of semivolatile
monomers can match the CLOUD growth rates with substantially lower SOA mass
yields; this is because the lighter monomers have a higher velocity and thus
a higher condensation rate for a given mass concentration. The
oligomerization simulations are a closer match to the CMU experiments than
the base-case simulations, though they overpredict the observations somewhat.
However, we also find that if the chemical conditions in CLOUD and the CMU
chamber were identical, substantial nucleation would have occurred in the CMU
experiments when in fact none occurred. This suggests that the chemical
mechanisms differed in the two experiments, perhaps because the high
oxidation rates in the SOA formation experiments led to rapid termination of
peroxy radical chemistry.
| Reference Key |
chuang2017atmosphericdynamic
Use this key to autocite in the manuscript while using
SciMatic Manuscript Manager or Thesis Manager
|
|---|---|
| Authors | ;W. K. Chuang;N. M. Donahue |
| Journal | Journal of agricultural and food chemistry |
| Year | 2017 |
| DOI |
10.5194/acp-17-10019-2017
|
| URL | |
| Keywords |
Citations
No citations found. To add a citation, contact the admin at info@scimatic.org
Comments
No comments yet. Be the first to comment on this article.