Specific features of phase equilibriums in Ln–Ba–Fe–O systems

Formation of five-layered Ln 2–ε Ba 3+ε Fe 5 O 15–δ phases [exhibiting nanoscale ordering with layer-by-layer location of the cations in the Ln–Ba–(Ln,Ba)–(Ln,Ba)–Ba–Ln perovskite-type structure] has occurred in the Ln–Ba–Fe–O (Ln = Y, Pr, Nd, Sm, Eu, and Gd) systems at 1100°С in air. Partial substi...

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Veröffentlicht in:Russian journal of general chemistry 2016-08, Vol.86 (8), p.1800-1804
Hauptverfasser: Volkova, N. E., Urusova, A. S., Gavrilova, L. Ya, Bryuzgina, A. V., Deryabina, K. M., Mychinko, M. Yu, Lebedev, O. I., Raveau, B., Cherepanov, V. A.
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container_end_page 1804
container_issue 8
container_start_page 1800
container_title Russian journal of general chemistry
container_volume 86
creator Volkova, N. E.
Urusova, A. S.
Gavrilova, L. Ya
Bryuzgina, A. V.
Deryabina, K. M.
Mychinko, M. Yu
Lebedev, O. I.
Raveau, B.
Cherepanov, V. A.
description Formation of five-layered Ln 2–ε Ba 3+ε Fe 5 O 15–δ phases [exhibiting nanoscale ordering with layer-by-layer location of the cations in the Ln–Ba–(Ln,Ba)–(Ln,Ba)–Ba–Ln perovskite-type structure] has occurred in the Ln–Ba–Fe–O (Ln = Y, Pr, Nd, Sm, Eu, and Gd) systems at 1100°С in air. Partial substitution of iron with cobalt (Ln 2–ε Ba 3+ε Fe 5– y Co y O 15–δ , Ln = Nd, Sm, Eu) has stabilized formation of the ordered structure. The oxygen content in the complex oxides has been determined in air over a wide temperature range by means of high-temperature thermogravimetry and iodometric titration. The change in oxygen content with temperature for the phases with five-layered ordering was significantly smaller than for the disordered phases.
doi_str_mv 10.1134/S1070363216080041
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subjects Chemical Sciences
Chemistry
Chemistry and Materials Science
Chemistry/Food Science
Cristallography
Gadolinium
High temperature
Iron
Material chemistry
or physical chemistry
Oxygen
Oxygen content
Perovskite structure
Perovskites
Phases
Theoretical and
Thermogravimetry
Titration
title Specific features of phase equilibriums in Ln–Ba–Fe–O systems
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