Pressure-induced antiferromagnet-ferromagnet transition and a change in the spin state of Co in La0.5Ba0.5CoO2.8

被引:5
|
作者
Kozlenko, D. P. [1 ]
Rutkauskas, A. V. [1 ]
Dang, N. T. [2 ]
Golosova, N. O. [1 ]
Kichanov, S. E. [1 ]
Dubrovinsky, L. S. [3 ]
Liermann, H. -P. [4 ]
Morgenroth, W. [5 ]
Savenko, B. N. [1 ]
机构
[1] Joint Inst Nucl Res, Dubna 141980, Moscow Region, Russia
[2] Duy Tan Univ, Inst Res & Dev, Da Nang 550000, Vietnam
[3] Univ Bayreuth, Bayer Geoinst, D-95440 Bayreuth, Germany
[4] DESY, D-22607 Hamburg, Germany
[5] Goethe Univ Frankfurt, Inst Geosci, D-60438 Frankfurt, Germany
基金
俄罗斯基础研究基金会;
关键词
Magnetic State; High Spin; Spin State; JETP Letter; Ferromagnetic State;
D O I
10.1134/S0021364014180052
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
The crystal and magnetic structures of anion-deficit cobaltite La0.5Ba0.5CoO2.8 have been studied by the X-ray and neutron diffraction methods at high pressures up to 30 and 6 GPa, respectively. A structure transition from the cubic phase with symmetry to the tetragonal phase with symmetry P4/mmm has been observed in this compound at P a parts per thousand 3 GPa. It is accompanied by the change of the ground antiferromagnetic state of the G type to the ferromagnetic state because of a change in the electronic configuration of Co3+ ions. Possible mechanisms of the observed magnetic phase transition, as well as the role of the superexchange interactions between Co3+ ions in various spin states in the formation of magnetic properties, have been discussed. Pressure-induced change in the magnetic state of La0.5Ba0.5CoO2.8 significantly differs from related stoichiometric compounds La(0.5)A(0.5)CoO(3.0) (A = Sr, Ca), where the ground ferromagnetic state is formed and the sign of the pressure dependence of the Curie temperature depends on the element A.
引用
收藏
页码:380 / 384
页数:5
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