Part X - The 1967 Howe Memorial Lecture – Iron and Steel Division - Thermodynamic Conditions for Spinodal Decomposition in a Multicomponent System

The American Institute of Mining, Metallurgical, and Petroleum Engineers
G. Bernard R. Hocine C. H. P. Lupis
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
5
File Size:
1216 KB
Publication Date:
Jan 1, 1968

Abstract

The necessary and sufficient conditions for the stability of a multicomponent phase with respect to infinitesinzal fluctuations are derived and transformed to be written in terms of activity coeffcients and mole fractions rather than in terms of the customary second deritlatives of the free energy. NECESSARY conditions for the stability of a multi-component system were derived by Gibbs as early as 1876.' However, as the usefulness of these conditions is greatly enhanced by the simplicity of their translation in terms of functions of common usage, the present contribution establishes these conditions in terms of activities or activity coefficients-and mole fractions. It was shown in another article2 that not only may these conditions be used for the prediction of the appearance of new phases, but they may also provide a check on the orders of magnitude of the interaction coefficients involved. "Spinodal" decomposition is said to occur when, at constant temperature and pressure, the system is unstable with respect to infinitesimal fluctuations in composition. As a result, the "phases" which appear may be attained through continuous changes in the system rather than discontinuous ones, and, consequently, the free energy of these phases may be described by a unique continuous free-energy function. For a binary system, the familiar curve of Fig. 1 illustrates the case we wish to extend to a multicom-ponent system. The conditions to be written pertain to the decomposition of a system of n moles into moles of phase moles of phase v, ...hen moles of phase 9, where the phases a, ...v, ...9 are—at least initially-arbitrarily close in composition to that of the original phase. Each A, is positive and since the total number of moles n in the system remains constant: Each phase v contains hv(nl +dnY) moles of component (I), ...xV(ni +dny) of component + dnk) moles of component (m). The total number of moles ni in the system remaining also constant, it is clear that:
Citation

APA: G. Bernard R. Hocine C. H. P. Lupis  (1968)  Part X - The 1967 Howe Memorial Lecture – Iron and Steel Division - Thermodynamic Conditions for Spinodal Decomposition in a Multicomponent System

MLA: G. Bernard R. Hocine C. H. P. Lupis Part X - The 1967 Howe Memorial Lecture – Iron and Steel Division - Thermodynamic Conditions for Spinodal Decomposition in a Multicomponent System. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1968.

Export
Purchase this Article for $25.00

Create a Guest account to purchase this file
- or -
Log in to your existing Guest account