A study of phase evolution of Fe-doped bismuth tantalate pyrochlore

被引:1
|
作者
Zhuk, N. A. [1 ]
Makeev, B. A. [2 ]
Korolev, R. I. [1 ]
Sivkov, D. N. [3 ]
Shpynova, A. D. [1 ]
机构
[1] Syktyvkar State Univ, Oktyabrsky Prospect 55, Syktyvkar 167001, Russia
[2] RAS, Inst Geol Komi Sci Ctr, UB, Pervomaiskaya st 48, Syktyvkar 167982, Russia
[3] RAS, Inst Phys, Math Komi Sci Ctr, UB, Oplesnina St 4, Syktyvkar 167982, Russia
关键词
Pyrochlore; Phase evolution; Iron; Ceramics; SYSTEM; EQUILIBRIA;
D O I
10.1016/j.ceramint.2022.07.132
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
The phase formation process of Bi2FeTa2O9.5 (sp. gr. Fd-3m) synthesized by traditional ceramic technology was studied. Bismuth orthotantalate BiTaO4 (sp. gr. Pnna) was found to be the precursor of the pyrochlore phase. The high-temperature synthesis of the iron-containing pyrochlore and the formation of a characteristic dendrite-like microstructure took place at temperatures above 900 degrees C. The pure pyrochlore was obtained at a temperature of 1050 degrees C. At the early stages of calcination, at a temperature close to 650 degrees C, the main part of iron (III) oxide, as a precursor, interacts with bismuth tantalate, and at temperatures above 950 degrees C, no Fe2O3 traces in the sample were found. Complex oxides Bi25FeO40 (sp. gr. I23), Bi3TaO7 (sp. gr. Fm-3m) were found as intermediate phases during the synthesis of pyrochlore. Pyrochlore of the given composition Bi2FeTa2O9.5 had a porous microstructure with a grain size of 0.5-1.0 mu m. The calcination temperature did not significantly affect the microstructure of the sample. The porosity of synthesized samples with a pyrochlore structure does not exceed 21%.
引用
收藏
页码:31965 / 31969
页数:5
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