Summary
-
1.
The phase diagrams of the binary systems Dy2O3-SiO2 and Er2O3-SiO2 were studied and constructed.
-
2.
Compounds of the types oxyorthosilicates (Dy2O[SiO4] and Er2O[SiO4), orthosilicates (Dy4[SiO4]3 and Er4SiO4 3), and pyrosilicates zed. The properties of these compounds were studied.
-
3.
The compound Er2[Si2O7], in contrast to other pyrosilicates of rare earth elements with atomic number lower than that of erbium, melts without decomposition and has higher birefringence.
-
4.
The limits of the separation regions in the studied systems were established, and their upper critical points were determined.
-
5.
Dysprosium oxide polymorphism was detected. Erbium oxide is not polymorphic.
Similar content being viewed by others
Literature cited
N. A. Toropov and I. A. Bondar', Izv. AN SSSR. Otd. Khim. n. 153 (1960).
N. A. Toropov, F. Ya. Galakhov, and S. F. Konovalova, Izv. AN SSSR. Otd. Khim. n. 539 (1961).
N. A. Toropov and I. A. Bondar', Izv. AN SSSR. Otd. Khim. n. 544 (1961).
N. A. Toropov and I. A. Bondar', Izv. AN SSSR. Otd. Khim. n. 739 (1961).
C. E. Curtis and J. R. Johnson, J. Am. Ceram. Soc.40, 1 (1957).
M. W. Shafer and R. Roy, J. Am. Ceram. Soc.42, 11 (1959).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Toropov, N.A., Galakhov, F.Y. & Konovalova, S.F. Silicates of the rare earth elements communication 5. phase diagrams of the Dy2O3-SiO2 and Er2O3-SiO2 systems. Russ Chem Bull 10, 1271–1277 (1961). https://doi.org/10.1007/BF00910094
Received:
Issue Date:
DOI: https://doi.org/10.1007/BF00910094