Magnetic phase transition in La0.8Sr0.2Mn0.9Sb0.1O3 manganite under pressure

被引:4
|
作者
Kichanov, S. E. [1 ]
Kozlenko, D. P. [1 ]
Khiem, L. H. [2 ]
Nghia, N. X. [2 ]
Lieu, N. T. T. [3 ]
Vu, M. T. [4 ]
Lukin, E., V [1 ]
Khan, D. T. [5 ]
Tuan, N. Q. [5 ]
Savenko, B. N. [1 ]
Dang, N. T. [6 ]
机构
[1] JINR, Frank Lab Neutron Phys, Dubna 141980, Moscow Reg, Russia
[2] Vietnam Acad Sci & Technol, Inst Phys, Hanoi 100000, Vietnam
[3] Posts & Telecommun Inst Technol, Hanoi 100000, Vietnam
[4] Univ Ulsan, Dept Phys, Ulsan 44610, South Korea
[5] Univ Danang Univ Sci & Educ, Da Nang 550000, Vietnam
[6] Duy Tan Univ, Inst Res & Dev, Da Nang 550000, Vietnam
关键词
Manganites; Neutron diffraction; High pressure; Magnetic phase separation; ARMCHAIR GRAPHENE NANORIBBONS; INDUCED ANTIFERROMAGNETISM; CRYSTAL; DOPANT;
D O I
10.1016/j.chemphys.2019.110541
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The high-pressure evolution of structural and magnetic properties of the single valence Mn3+ manganite La0.8Sr0.2Mn0.9Sb0.1O3 was studied by means of neutron powder diffraction up to 4.5 GPa in the temperature range of 10-300 K. At ambient pressure, a ferromagnetic ground state with the magnetic ordering temperature T-C approximate to 175 K is stabilized. Application of high pressure suppresses the initial FM phase and leads to the appearance of a new A-type antiferromagnetic AFM phase with T-N similar to 130 K at P = 2.2 GPa. Under compression, both T-C and T-N almost linearly increases with the pressure coefficient of 1.9(2) and 0.9(3) K/GPa, respectively. It is assumed that the appearance of the A-type AFM state is mediated by the strong anisotropic distortions of MnO6 octahedra, coupled to the e(g)d(x2-z2) orbital polarization at high pressures.
引用
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页数:5
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