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Homogeneous water nucleation in a laminar flow diffusion chamber
Homogeneous nucleation rates of water at temperatures between 240 and 270 K were measured in a laminar flow diffusion chamber at ambient pressure and helium as carrier gas. Being in the range of 10 2 - 10 6 cm − 3 s − 1 , the experimental results extend the nucleation rate data from literature con...
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Published in: | The Journal of chemical physics 2010-06, Vol.132 (24), p.244505-244505-6 |
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Main Authors: | , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Homogeneous nucleation rates of water at temperatures between 240 and 270 K were measured in a laminar flow diffusion chamber at ambient pressure and helium as carrier gas. Being in the range of
10
2
-
10
6
cm
−
3
s
−
1
, the experimental results extend the nucleation rate data from literature consistently and fill a pre-existing gap. Using the macroscopic vapor pressure, density, and surface tension for water we calculate the nucleation rates predicted by classic nucleation theory (CNT) and by the empirical correction function of CNT by
Wölk
and
Strey
[
J. Phys. Chem. B
105
,
11683
(
2001
)]
. As in the case of other systems (e.g., alcohols), CNT predicts a stronger temperature dependence than experimentally observed, whereas the agreement with the empirical correction function is good for all data sets. Furthermore, the isothermal nucleation rate curves allow us to determine the experimental critical cluster sizes by use of the nucleation theorem. A comparison with the critical cluster sizes calculated by use of the Gibbs-Thomson equation is remarkably good for small cluster sizes, for bigger ones the Gibbs-Thomson equation overestimates the cluster sizes. |
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ISSN: | 0021-9606 1089-7690 |
DOI: | 10.1063/1.3427537 |