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Proceedings of the National Academy of Sciences of the United States of America logoLink to Proceedings of the National Academy of Sciences of the United States of America
. 1972 Nov;69(11):3428–3431. doi: 10.1073/pnas.69.11.3428

Fluidity: A General Theory

J H Hildebrand 1, R H Lamoreaux 1
PMCID: PMC389786  PMID: 16592031

Abstract

The equation ϕ = B(V - Vo)/Vo, which reproduces the fluidity of simple liquids accurately over ranges between freezing and boiling points, is here shown to hold to pressures of at least 500 atm, and nearly to critical volumes. Fluidity can vary continuously above the critical region into that of compressed gas, where the parameter B becomes a function of temperature.

The parameter Vo is a “corresponding states” fraction of the critical molal volume. It is identical with the molal volume of the solid only in cases where molecules are free to rotate as they do in the liquid.

Parameter B is a measure of the extent to which the external momentum that produces viscous flow is absorbed by the molecules of the liquid. Such damping can result from molecular mass, e.g., Ne, Ar, Kr; flexibility, normal alkanes; or rotational inertia, SiBr4 against SiCl4.

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Selected References

These references are in PubMed. This may not be the complete list of references from this article.

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