2019
DOI: 10.1021/acs.chemmater.9b02716
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Multiferroism Induced by Spontaneous Structural Ordering in Antiferromagnetic Iron Perovskites

Abstract: Room-temperature multiferroism in polycrystalline antiferromagnetic Fe perovskites is reported for the first time. In the perovskite-type oxides RE 1.2 Ba 1.2 Ca 0.6 Fe 3 O 8 (RE = Gd, Tb), the interplay of layered ordering of Gd(Tb), Ba, and Ca atoms with the ordering of FeO 4 -tetrahedra (T) and FeO 6 -octahedra (O) results in a polar crystal structure. The layered structure consists of the stacking sequence of RE/Ca-RE/Ca-Ba-RE/Ca layers in combination with the TOOT sequence in a unit cell. A polar moment o… Show more

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Cited by 8 publications
(36 citation statements)
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“…Substitution of RE by Ca in the systems modifies the layered ordering of these cations and the oxygen content in such a way that the RE 3+ , Ba 2+ , and Ca 2+ ordering is established in blocks of 3 a p periodicity in the RE 1.2 Ba 1.2 Ca 0.6 Fe 3 O 8 oxides; in blocks of 5 a p periodicity in the REBa 2 Ca 2 Fe 5 O 13 oxides; and by intercalation of blocks of 3 a p and 5 a p periodicity in the intermediate RE 2.2 Ba 3.2 Ca 2.6 Fe 8 O 21 compounds. 17 , 18 The different RE 3+ , Ba 2+ , and Ca 2+ ordering drives the formation of the different Fe-coordination polyhedra (tetrahedron, octahedron, and square pyramid) and their different layered ordering leading to the current structures. 17 , 18 …”
Section: Resultsmentioning
confidence: 99%
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“…Substitution of RE by Ca in the systems modifies the layered ordering of these cations and the oxygen content in such a way that the RE 3+ , Ba 2+ , and Ca 2+ ordering is established in blocks of 3 a p periodicity in the RE 1.2 Ba 1.2 Ca 0.6 Fe 3 O 8 oxides; in blocks of 5 a p periodicity in the REBa 2 Ca 2 Fe 5 O 13 oxides; and by intercalation of blocks of 3 a p and 5 a p periodicity in the intermediate RE 2.2 Ba 3.2 Ca 2.6 Fe 8 O 21 compounds. 17 , 18 The different RE 3+ , Ba 2+ , and Ca 2+ ordering drives the formation of the different Fe-coordination polyhedra (tetrahedron, octahedron, and square pyramid) and their different layered ordering leading to the current structures. 17 , 18 …”
Section: Resultsmentioning
confidence: 99%
“… 17 , 18 The different RE 3+ , Ba 2+ , and Ca 2+ ordering drives the formation of the different Fe-coordination polyhedra (tetrahedron, octahedron, and square pyramid) and their different layered ordering leading to the current structures. 17 , 18 …”
Section: Resultsmentioning
confidence: 99%
See 3 more Smart Citations