Bilde, Merete, Barsanti, Kelley, Booth, Murray, Cappa, Christopher D., Donahue, Neil M., Emanuelsson, Eva U., McFiggans, Gordon, Krieger, Ulrich K., Marcolli, Claudia, Topping, David, Ziemann, Paul, Barley, Mark, Clegg, Simon, Dennis-Smither, Benjamin, Hallquist, Mattias, Hallquist, Åsa M., Khlystov, Andrey, Kulmala, Markku, Mogensen, Ditte, Percival, Carl J., Pope, Francis, Reid, Jonathan P., Ribeiro Da Silva, M. A V, Rosenoern, Thomas, Salo, Kent, Soonsin, Vacharaporn Pia, Yli-Juuti, Taina, Prisle, Nonne L., Pagels, Joakim, Rarey, Juergen, Zardini, Alessandro A. and Riipinen, Ilona (2015) Saturation vapor pressures and transition enthalpies of low-volatility organic molecules of atmospheric relevance:From dicarboxylic acids to complex mixtures. Chemical Reviews, 115 (10). pp. 4115-4156. ISSN 0009-2665
Full text not available from this repository. (Request a copy)Abstract
There are a number of techniques that can be used that differ in terms of whether they fundamentally probe the equilibrium and the temperature range over which they can be applied. The series of homologous, straight-chain dicarboxylic acids have received much attention over the past decade given their atmospheric relevance, commercial availability, and low saturation vapor pressures, thus making them ideal test compounds. Uncertainties in the solid-state saturation vapor pressures obtained from individual methodologies are typically on the order of 50-100%, but the differences between saturation vapor pressures obtained with different methods are approximately 1-4 orders of magnitude, with the spread tending to increase as the saturation vapor pressure decreases. Some of the dicarboxylic acids can exist with multiple solid-state structures that have distinct saturation vapor pressures. Furthermore, the samples on which measurements are performed may actually exist as amorphous subcooled liquids rather than solid crystalline compounds, again with consequences for the measured saturation vapor pressures, since the subcooled liquid phase will have a higher saturation vapor pressure than the crystalline solid phase. Compounds with equilibrium vapor pressures in this range will exhibit the greatest sensitivities in terms of their gas to particle partitioning to uncertainties in their saturation vapor pressures, with consequent impacts on the ability of explicit and semiexplicit chemical models to simulate secondary organic aerosol formation.
Item Type: | Article |
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Uncontrolled Keywords: | chemistry(all) ,/dk/atira/pure/subjectarea/asjc/1600 |
Faculty \ School: | Faculty of Science > School of Environmental Sciences |
UEA Research Groups: | Faculty of Science > Research Groups > Centre for Ocean and Atmospheric Sciences |
Related URLs: | |
Depositing User: | Pure Connector |
Date Deposited: | 16 Feb 2017 02:24 |
Last Modified: | 21 Oct 2022 10:30 |
URI: | https://ueaeprints.uea.ac.uk/id/eprint/62630 |
DOI: | 10.1021/cr5005502 |
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