Magnetic properties and energy-mapping analysis

被引:408
作者
Xiang, Hongjun [1 ,2 ]
Lee, Changhoon [3 ]
Koo, Hyun-Joo [4 ,5 ]
Gong, Xingao [1 ,2 ]
Whangbo, Myung-Hwan [3 ]
机构
[1] Fudan Univ, State Key Lab Surface Phys, Key Lab Computat Phys Sci, Minist Educ, Shanghai 200433, Peoples R China
[2] Fudan Univ, Dept Phys, Shanghai 200433, Peoples R China
[3] N Carolina State Univ, Dept Chem, Raleigh, NC 27695 USA
[4] Kyung Hee Univ, Dept Chem, Seoul 130701, South Korea
[5] Kyung Hee Univ, Res Inst Basic Sci, Seoul 130701, South Korea
关键词
SPIN-EXCHANGE INTERACTIONS; DENSITY-FUNCTIONAL ANALYSIS; CLASSICAL SPIN; HARTREE-FOCK; IRON-OXIDE; HEISENBERG; CHAIN; ANTIFERROMAGNETISM; FERROMAGNETISM; INCOMMENSURATE;
D O I
10.1039/c2dt31662e
中图分类号
O61 [无机化学];
学科分类号
070301 ; 081704 ;
摘要
The magnetic energy levels of a given magnetic solid are closely packed in energy because the interactions between magnetic ions are weak. Thus, in describing its magnetic properties, one needs to generate its magnetic energy spectrum by employing an appropriate spin Hamiltonian. In this review article we discuss how to determine and specify a necessary spin Hamiltonian in terms of first principles electronic structure calculations on the basis of energy-mapping analysis and briefly survey important concepts and phenomena that one encounters in reading the current literature on magnetic solids. Our discussion is given on a qualitative level from the perspective of magnetic energy levels and electronic structures. The spin Hamiltonian appropriate for a magnetic system should be based on its spin lattice, i.e., the repeat pattern of its strong magnetic bonds (strong spin exchange paths), which requires one to evaluate its Heisenberg spin exchanges on the basis of energy-mapping analysis. Other weaker energy terms such as Dzyaloshinskii-Moriya (DM) spin exchange and magnetocrystalline anisotropy energies, which a spin Hamiltonian must include in certain cases, can also be evaluated by performing energy-mapping analysis. We show that the spin orientation of a transition-metal magnetic ion can be easily explained by considering its split d-block levels as unperturbed states with the spin-orbit coupling (SOC) as perturbation, that the DM exchange between adjacent spin sites can become comparable in strength to the Heisenberg spin exchange when the two spin sites are not chemically equivalent, and that the DM interaction between rare-earth and transition-metal cations is governed largely by the magnetic orbitals of the rare-earth cation.
引用
收藏
页码:823 / 853
页数:31
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