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Determination of the evaporation coefficient of D2O

Bibliographic Details
Title: Determination of the evaporation coefficient of D2O
Authors: R. C. Cohen, R. J. Saykally, J. D. Smith, C. D. Cappa, W. S. Drisdell
Source: Atmospheric Chemistry and Physics, Vol 8, Iss 22, Pp 6699-6706 (2008)
Publisher Information: Copernicus Publications, 2008.
Publication Year: 2008
Collection: LCC:Physics
LCC:Chemistry
Subject Terms: Physics, QC1-999, Chemistry, QD1-999
More Details: The evaporation rate of D2O has been determined by Raman thermometry of a droplet train (12–15 μm diameter) injected into vacuum (~10-5 torr). The cooling rate measured as a function of time in vacuum was fit to a model that accounts for temperature gradients between the surface and the core of the droplets, yielding an evaporation coefficient (γe) of 0.57±0.06. This is nearly identical to that found for H2O (0.62±0.09) using the same experimental method and model, and indicates the existence of a kinetic barrier to evaporation. The application of a recently developed transition-state theory (TST) model suggests that the kinetic barrier is due to librational and hindered translational motions at the liquid surface, and that the lack of an isotope effect is due to competing energetic and entropic factors. The implications of these results for cloud and aerosol particles in the atmosphere are discussed.
Document Type: article
File Description: electronic resource
Language: English
ISSN: 1680-7316
1680-7324
Relation: http://www.atmos-chem-phys.net/8/6699/2008/acp-8-6699-2008.pdf; https://doaj.org/toc/1680-7316; https://doaj.org/toc/1680-7324
Access URL: https://doaj.org/article/2214addea9594ed09a96410d1b97056a
Accession Number: edsdoj.2214addea9594ed09a96410d1b97056a
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  Data: Atmospheric Chemistry and Physics, Vol 8, Iss 22, Pp 6699-6706 (2008)
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  Data: The evaporation rate of D2O has been determined by Raman thermometry of a droplet train (12–15 μm diameter) injected into vacuum (~10-5 torr). The cooling rate measured as a function of time in vacuum was fit to a model that accounts for temperature gradients between the surface and the core of the droplets, yielding an evaporation coefficient (γe) of 0.57±0.06. This is nearly identical to that found for H2O (0.62±0.09) using the same experimental method and model, and indicates the existence of a kinetic barrier to evaporation. The application of a recently developed transition-state theory (TST) model suggests that the kinetic barrier is due to librational and hindered translational motions at the liquid surface, and that the lack of an isotope effect is due to competing energetic and entropic factors. The implications of these results for cloud and aerosol particles in the atmosphere are discussed.
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