Subsolidus Phase Equilibrium Study of the Ternary Systems Li2O–Nd2O3–GeO2and –SiO2

1984 ◽  
Vol 23 (Part 1, No. 7) ◽  
pp. 815-819
Author(s):  
Takuro Ikeda ◽  
Hidetaka Sato
2015 ◽  
Vol 47 (1) ◽  
pp. 164-173 ◽  
Author(s):  
Hongquan Liu ◽  
Zhixiang Cui ◽  
Mao Chen ◽  
Baojun Zhao

JOM ◽  
2020 ◽  
Vol 72 (9) ◽  
pp. 3204-3212 ◽  
Author(s):  
Junjie Shi ◽  
Min Chen ◽  
Xingbang Wan ◽  
Pekka Taskinen ◽  
Ari Jokilaakso

Author(s):  
R. S. Bradley ◽  
P. Engel ◽  
D. C. Munro

SummaryThe subsolidus phase equilibrium of the lithiophilite-tephroite system was studied in the temperature range 500 to 900° C. The solubility of tephroite in lithiophilite is limited and increases with temperature. The reaction is very sluggish and has peculiar kinetic properties. No reverse solubility was observed. Similar asymmetry was found in the LiMgPO4-forsterite system of which a preliminary study was made. Apparent absences of silicate phosphate olivine solid solutions in nature are related to our experimental findings and to geological factors.


1987 ◽  
Vol 42 (8) ◽  
pp. 1052-1053
Author(s):  
Gerd Seemann ◽  
Karl Hensen

AbstractA phase equilibrium study of the system aluminiumbromide and pyridiniumbromide has been carried out. The phase diagram of the system indicates the existence of three congruently melting com pounds of the molar ratio AlBr3/PyHBr 1:1, 1:3, 2 :3 and one incongruently melting compound of the molar ratio 1:2 and is therefore similar to the AlCl3-PyHCl system [1].


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