MISCIBILITY GAP BETWEEN FES AND FE1-XS

被引：20

作者：

YUND, RA

HALL, HT

机构：

[1] Department of Geological Sciences Brown University Providence, RI

来源：

MATERIALS RESEARCH BULLETIN | 1968年 / 3卷 / 09期

关键词：

D O I：

10.1016/0025-5408(68)90047-0

中图分类号：

T [工业技术];

学科分类号：

08 ;

摘要：

The miscibility gap between FeS (troilite) and Fe1-xS (pyrrhotite) below 140°C has been confirmed. Troilite is restricted to essentially stoichiometric FeS, and the composition of pyrrhotite in equilibrium with troilite can be expressed by the relation ln (C - 48.00) = 9.4±0.4 -(3.6±0.2 × 103) T, where C is the composition of pyrrhotite in atomic percent iron and T is ok. © 1968.

引用

页码：779 / &

共 13 条

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