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Constitution of Bone China: III, High‐Temperature Phase Equilibrium Studies in the System Tricalcium PhosphateAnorthite‐Silica
Author(s) -
PIERRE P. D. S. ST.
Publication year - 1956
Publication title -
journal of the american ceramic society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.9
H-Index - 196
eISSN - 1551-2916
pISSN - 0002-7820
DOI - 10.1111/j.1151-2916.1956.tb14181.x
Subject(s) - anorthite , eutectic system , mineralogy , ternary operation , ternary numeral system , phase (matter) , phosphate , materials science , chemistry , metallurgy , microstructure , organic chemistry , computer science , programming language
The primary‐phase fields of the system tricalcium phosphate‐anorthite‐silica are delineated, and the distribution of isotherms is related to the firing of bone china. The system is a true ternary with a eutectic at 11% tricalcium phosphate, 51% anorthite, 38% silica that melts at 1290°± 5°C.