Spin order in the charge disproportionated phases of the A-site layer ordered triple perovskite LaCa2Fe3O9

被引:7
|
作者
Arevalo-Lopez, Angel M. [1 ]
Hosaka, Yoshiteru [2 ]
Guo, Haichuan [2 ]
Romero, Fabio Denis [2 ,3 ]
Saito, Takashi [2 ]
Attfield, J. Paul [4 ,5 ]
Shimakawa, Yuichi [2 ]
机构
[1] Univ Lille, CNRS, Cent Lille, ENSCL,Univ Artois,UCCS,UMR 8181, F-59000 Lille, France
[2] Kyoto Univ, Inst Chem Res, Kyoto 6110011, Japan
[3] Kyoto Univ, Hakubi Ctr Adv Res, Sakyo Ku, Yoshida Honmachi, Kyoto 6068501, Japan
[4] Univ Edinburgh, Ctr Sci Extreme Condit, Peter Guthrie Tait Rd,Kings Bldg, Edinburgh EH9 3FD, Midlothian, Scotland
[5] Univ Edinburgh, Sch Chem, Peter Guthrie Tait Rd,Kings Bldg, Edinburgh EH9 3FD, Midlothian, Scotland
基金
日本学术振兴会; 英国工程与自然科学研究理事会; 日本科学技术振兴机构;
关键词
TRANSITION POINT;
D O I
10.1103/PhysRevB.97.024421
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
The coupling between spins and charge disproportionation states has been investigated in the LaCa2Fe3O9 oxide with neutron powder diffraction. This A-site layer ordered triple perovskite LaCa2Fe3O9 undergoes charge disproportionation on cooling and shows two different charge ordering patterns. At 230 K, Fe3.67+ disproportionates into a 2:1 ratio of Fe3+ : Fe5+, which order in a layered manner along the < 010 > direction of the pseudocubic unit cell. At lower temperatures (T < 170 K), the charge ordering pattern changes to a layered arrangement along the < 111 > direction. Neutron powder diffraction data show that in the intermediate temperature range (170 K < T < 230 K) the spins order into a cycloidal structure on the ac plane for the Fe3+ cations while the Fe5+ cations remain paramagnetic. For the lowest temperature range (2K < T < 190 K), the spin structure follows the charge ordering and evolves to a < 111 > layered magnetic structure.
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页数:5
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