Effect of secondary organic aerosol coating thickness on the real-time detection and characterization of biomass-burning soot by two particle mass spectrometers
Clicks: 474
ID: 56524
2016
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
Steady Performance
65.9
/100
474 views
336 readers
Trending
AI Quality Assessment
Not analyzed
Readership in this journal
SteadyRanked #2 of 28 articles by views in atmospheric measurement techniques
Most read
Least read
Bar heights use a square-root scale.
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
Biomass burning is a large source of light-absorbing refractory black carbon
(rBC) particles with a wide range of morphologies and sizes. The net
radiative forcing from these particles is strongly dependent on the amount
and composition of non-light-absorbing material internally mixed with the rBC
and on the morphology of the mixed particles. Understanding how the mixing
state and morphology of biomass-burning aerosol evolves in the atmosphere is
critical for constraining the influence of these particles on radiative
forcing and climate. We investigated the response of two commercial
laser-based particle mass spectrometers, the vacuum ultraviolet (VUV)
ablation LAAPTOF
and the IR vaporization SP-AMS, to monodisperse biomass-burning particles as
we sequentially coated the particles with secondary organic aerosol (SOA)
from α-pinene ozonolysis. We studied three mobility-selected soot
core sizes, each with a number of successively thicker coatings of SOA
applied. Using IR laser vaporization, the SP-AMS had different changes in
sensitivity to rBC compared to potassium as a function of applied SOA
coatings. We show that this is due to different effective beam widths for
the IR laser vaporization region of potassium versus black carbon. The
SP-AMS's sensitivity to black carbon (BC) mass was not observed to plateau following
successive SOA coatings, despite achieving high OA : BC mass ratios greater than 9. We also measured the ion fragmentation pattern of
biomass-burning rBC and found it changed only slightly with increasing SOA
mass. The average organic matter ion signal measured by the LAAPTOF
demonstrated a positive correlation with the condensed SOA mass on
individual particles, despite the inhomogeneity of the particle core
compositions. This demonstrates that the LAAPTOF can obtain quantitative
mass measurements of aged soot-particle composition from realistic
biomass-burning particles with complex morphologies and composition.
| Reference Key |
ahern2016effectatmospheric
Use this key to autocite in the manuscript while using
SciMatic Manuscript Manager or Thesis Manager
|
|---|---|
| Authors | Ahern, A. T.;Subramanian, R.;Saliba, G.;Lipsky, E. M.;Lipsky, E. M.;Donahue, N. M.;Sullivan, R. C.; |
| Journal | atmospheric measurement techniques |
| Year | 2016 |
| DOI |
DOI not found
|
| 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.