A diagonal volatility basis set to assess the condensation of organic vapors onto particles
Creators
- Lopez, Brandon1
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Bhattacharyya, Nirvan1
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DeVivo, Jenna1
- Wang, Mingyi1, 2
- Caudillo-Plath, Lucia3
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Surdu, Mihnea4
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Bianchi, Federico5
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Brasseur, Zoé5
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Buchholz, Angela6
- Chen, Dexian1, 7
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Duplissy, Jonathan5
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He, Xu-Cheng5, 8
- Hofbauer, Victoria1
- Mahfouz, Naser1
- Makhmutov, Vladimir9, 10
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Marten, Ruby4
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Mentler, Bernhard11
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Philippov, Maxim9, 10
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Schervish, Meredith1
- Wang, Dongyu S.4
- Weber, Stefan K.3, 12
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Welti, André13
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El Haddad, Imad4
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Lehtipalo, Katrianne5
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Kulmala, Markku5
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Worsnop, Douglas5, 14
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Kirkby, Jasper3, 12
- Mauldin, Roy L.1, 15
- Stolzenburg, Dominik16, 17
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Schobesberger, Siegfried6
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Flagan, Richard18
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Donahue, Neil M.1
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1.
Carnegie Mellon University
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2.
University of Chicago
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3.
Goethe University Frankfurt
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4.
Paul Scherrer Institute
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5.
University of Helsinki
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6.
University of Eastern Finland
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7.
Sun Yat-sen University
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8.
University of Cambridge
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9.
P.N. Lebedev Physical Institute of the Russian Academy of Sciences
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10.
Moscow Institute of Physics and Technology
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11.
Universität Innsbruck
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12.
European Organization for Nuclear Research
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13.
Finnish Meteorological Institute
- 14. Aerodyne Inc, Billerica, MA, USA
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15.
University of Colorado Boulder
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16.
University of Vienna
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17.
TU Wien
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18.
California Institute of Technology
Abstract
We present a “diagonal” Volatility Basis Set (dVBS) comparing gas-phase concentrations of oxygenated organic molecules (OOM) to their condensed-phase mass fractions. This permits closure of vapor concentrations with particle composition constrained by particle growth rates, allowing the contributions of quasi non-volatile condensation, equilibrium partitioning, and reactive uptake to be separated. The dVBS accommodates both equilibrium and dynamical (growth) conditions. Growth implies an association between gas and particle concentrations governed by a “condensation line” that is set by the particle growth rate, which fixes the total (excess) concentration of condensible vapors. The condensation line defines an infeasible region of high particle mass fraction and low gas concentration; under steady-state growth conditions, compounds cannot appear in this infeasible region without being formed by condensed-phase chemistry. We test the dVBS with observations from the CLOUD experiment at CERN using data from a FIGAERO I− Chemical Ionization Mass Spectrometer measuring vapors directly and particle composition via temperature programmed desorption from a filter. A dVBS analysis finds that data from an α-pinene + O3 run at 243 K are consistent with volatility driven condensation forming the large majority of particle mass, with no compounds clearly within the infeasible region.
Copyright and License
© 2025 The Author(s). Published by the Royal Society of Chemistry. This article is licensed under a Creative Commons Attribution 3.0 Unported Licence.
Acknowledgement
This work was supported by: grants AGS1447056, AGS1439551, AGS1531284, AGS1801574, AGS1801897, AGS2132089, AGS2215489, AGS2431817, AGS2215527 and CHE2336463 from the U.S. National Science Foundation; the Wallace Research Foundation; the CMU Scott Institute for Energy Innovation; grant 42205108 from National Natural Science Foundation of China; project VRG22-003 from the Vienna Science and Technology Fund (WWF); grants PZ00P2_216181 and 200021_213071 from the Swiss National Foundation; and grants 346371 and 364229 from the Research Council of Finland.
Data Availability
Data for all figures in this paper are available on the CERN Zenodo server.
Files
d5ea00062a.pdf
Additional details
Identifiers
- PMCID
- PMC12314873
- PMID
- 40756074
Related works
- Describes
- Journal Article: PMC12314873 (PMCID)
- Journal Article: 40756074 (PMID)
Funding
- National Science Foundation
- AGS1447056
- National Science Foundation
- AGS1439551
- National Science Foundation
- AGS1531284
- National Science Foundation
- AGS1801574
- National Science Foundation
- AGS1801897
- National Science Foundation
- AGS2132089
- National Science Foundation
- AGS2215489
- National Science Foundation
- AGS2431817
- National Science Foundation
- AGS2215527
- National Science Foundation
- CHE2336463
- Wallace Research Foundation
- Carnegie Mellon University
- CMU Scott Institute for Energy Innovation -
- National Natural Science Foundation of China
- 42205108
- Vienna Science and Technology Fund
- VRG22-003
- Swiss National Science Foundation
- PZ00P2_216181
- Swiss National Science Foundation
- 200021_213071
- Research Council of Finland
- 346371
- Research Council of Finland
- 364229
Dates
- Accepted
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2025-07-20
- Available
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2025-07-21Published online