Evidence map›Paper›PMID 27791063›Full record

ArticleProceedings of the National Academy of Sciences of the United States of America2016

Lability of secondary organic particulate matter.

Pengfei Liu, Yong Jie Li, Yan Wang, Mary K Gilles, Rahul A Zaveri, Allan K Bertram, Scot T Martin

Abstract read
In one paragraph

Article in Proceedings of the National Academy of Sciences of the United States of America, 2016. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 13 papers.

0numbers the graph read from it
0cells of the map it votes in
13citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

13 citing papers in PubMed.

  1. Article
  2. Article
  3. Article
  4. Article
  5. Article
  6. Article
  7. Toward a molecular understanding of the surface composition of atmospherically relevant organic particles.Proceedings of the National Academy of Sciences of the United States of America · 2022
    Article
  8. Article
  9. Article
  10. Review
  11. Article
  12. Article
  13. Mixing of secondary organic aerosols versus relative humidity.Proceedings of the National Academy of Sciences of the United States of America · 2016
    Article
4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

7 authors.

Pengfei LiuJohn A. Paulson School of Engineering and Applied Sciences, Harvard University, Cambridge, MA 02138.
Yong Jie LiJohn A. Paulson School of Engineering and Applied Sciences, Harvard University, Cambridge, MA 02138.
Yan WangJohn A. Paulson School of Engineering and Applied Sciences, Harvard University, Cambridge, MA 02138.
Mary K GillesChemical Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA 94720.
Rahul A ZaveriAtmospheric Sciences and Global Change Division, Pacific Northwest National Laboratory, Richland, WA 99354.
Allan K BertramDepartment of Chemistry, University of British Columbia, Vancouver, BC, Canada, VT6 1Z1.
Scot T MartinJohn A. Paulson School of Engineering and Applied Sciences, Harvard University, Cambridge, MA 02138; scot_martin@harvard.edu.ORCID http://orcid.org/0000-0002-5372-6214

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The energy flows in Earth's natural and modified climate systems are strongly influenced by the concentrations of atmospheric particulate matter (PM). For predictions of concentration, equilibrium partitioning of semivolatile organic compounds (SVOCs) between organic PM and the surrounding vapor has widely been assumed, yet recent observations show that organic PM can be semisolid or solid for some atmospheric conditions, possibly suggesting that SVOC uptake and release can be slow enough that equilibrium does not prevail on timescales relevant to atmospheric processes. Herein, in a series of laboratory experiments, the mass labilities of films of secondary organic material representative of similar atmospheric organic PM were directly determined by quartz crystal microbalance measurements of evaporation rates and vapor mass concentrations. There were strong differences between films representative of anthropogenic compared with biogenic sources. For films representing anthropogenic PM, evaporation rates and vapor mass concentrations increased above a threshold relative humidity (RH) between 20% and 30%, indicating rapid partitioning above a transition RH but not below. Below the threshold, the characteristic time for equilibration is estimated as up to 1 wk for a typically sized particle. In contrast, for films representing biogenic PM, no RH threshold was observed, suggesting equilibrium partitioning is rapidly obtained for all RHs. The effective diffusion rate

Indexed as

atmospheric chemistryevaporationsecondary organic aerosol

Identifiers

PMID27791063
PMCPMC5111713

What OpenQuestion holds

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Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.