Extractive Metallurgy Division - The Miscibility Gap in the System Ag-Fe-Pd at 1000°, 1100°, 1080 and 1200°C (TN)

- Organization:
- The American Institute of Mining, Metallurgical, and Petroleum Engineers
- Pages:
- 2
- File Size:
- 109 KB
- Publication Date:
- Jan 1, 1962
Abstract
PHASE relations in three isothermal sections (l000°, 1100°, 1200°C) of the system Ag-Fe-Pd have been determined as part of a program to develop improved crucible materials for containing low-melting iron silicates at low oxygen potentials. The following experimental method was used: Two- to 3- g samples of each of forty different alloys within the system Ag-Fe-Pd were made up from metals of 99.9 pct purity. The mixed metal powders were contained in a 1-cc crucible of dense recrystal-lized alumina and heated in a protective atmosphere (90 vol pct A, 10 vol pct H2), first to complete melting for approximately 30 min and subsequently at the desired equilibration temperature (1000°, 1100°, or 1200°C) for approximately 24 hr. The samples were then quenched rapidly to room temperature and examined metallographically as well as by X-ray techniques. Unit cell dimensions were compared with standards obtained by study of one-phase alloys of known compositions. The results are summarized in diagrams (a), (b), and (c) shown in Fig. 1. Heavy solid curves outline areas comprising compositions of mixtures consisting of the phases labeled for each area. Mixtures in which liquid is the only condensed phase present are confined to very narrow areas adjacent to the Ag-Pd join at high silver contents. An enlarged, distorted picture of the phase relations prevailing in these areas is shown in the upper-left circular insert. Particular attention is directed toward the misci-bility gap which occupies major parts of the composi-
Citation
APA:
(1962) Extractive Metallurgy Division - The Miscibility Gap in the System Ag-Fe-Pd at 1000°, 1100°, 1080 and 1200°C (TN)MLA: Extractive Metallurgy Division - The Miscibility Gap in the System Ag-Fe-Pd at 1000°, 1100°, 1080 and 1200°C (TN). The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1962.