MONTICELLITE AND FORSTERITE CRYSTALLINE SOLUTIONS

被引：26

作者：

BIGGAR, GM

OHARA, MJ

机构：

[1] Grant Institute of Geology, University of Edinburgh, Edinburgh

来源：

JOURNAL OF THE AMERICAN CERAMIC SOCIETY | 1969年 / 52卷 / 05期

关键词：

D O I：

10.1111/j.1151-2916.1969.tb09177.x

中图分类号：

TQ174 [陶瓷工业]; TB3 [工程材料学];

学科分类号：

0805 ; 080502 ;

摘要：

New data for monticellite crystalline solutions confirm that monticellite (CaMgSiO4 is unstable at atmospheric pressure. On the join forsterite‐monticellite, the estimated range of stable monticellite crystalline solutions is 89 to 93 mol% monticellite at 1200°C and 75 to 92 mol% at 1490°C. The range of forsterite crystalline solution is 93 to 100 mol% forsterite at 1200°C and 81 t0 100 mol% at 1490°C. These results can be applied to the proportions of phases present in impure periclase refractories at service temperatures. Copyright © 1969, Wiley Blackwell. All rights reserved

引用

页码：249 / &

共 8 条

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[8]

[No title captured]

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