首页> 外文期刊>Physical Review, B. Condensed Matter >AB INITIO CALCULATION OF ELECTRONIC STRUCTURE, CRYSTAL FIELD, AND INTRINSIC MAGNETIC PROPERTIES OF SM2FE17, SM2FE17N3, SM2FE17C3, AND SM2CO17
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AB INITIO CALCULATION OF ELECTRONIC STRUCTURE, CRYSTAL FIELD, AND INTRINSIC MAGNETIC PROPERTIES OF SM2FE17, SM2FE17N3, SM2FE17C3, AND SM2CO17

机译:从头计算SM2FE17,SM2FE17N3,SM2FE17C3和SM2CO17的电子结构,晶体场和本征磁性

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In a comparative study we calculated the spin and orbital moments, spin and charge densities, and 4f crystal field (CF) parameters of the rare-earth transition-metal intermetallics Sm(2)Fe(17)Z(3) (Z=C,N) and Sm2Co17 using a relativistic optimized linear combination of atomic orbitals method. The itinerant valence electron states were treated in the local-spin- density approximation (LSDA), whereas the localized 4f states were described as open core states within the self-interaction-corrected LSDA. The calculations yield magnetic moments in good agreement with experiment. While all local moments of Sm2Fe17 increase upon lattice expansion, the moments of atoms neighbouring the interstitial sites decrease and those of more distant Fe atoms increase upon insertion of interstitial N or C. In N interstitial atoms all 2p(alpha) orbitals are polarized antiparallel to their respective Fe and Sm neighbor atoms in the bond directions, whereas in C all 2p(alpha) orbitals are polarized antiparallel to the Fe atoms neighboring the interstitial site. The second-order CF parameters A(2)(0) dominating the rare-earth magnetocrystalline anisotropy are found to have the same sign and order of magnitude as those derived from magnetization data. In accordance with experiment the calculated negative A(2)(0) is larger for the Co compound than for the Fe parent compound and is largely strongly increased upon insertion of interstitial N or C. The agreement between theory and experiment is improved by taking into account the CF contribution arising from the asphericity of the exchange-correlation potential of the non-4f states. [References: 93]
机译:在一项比较研究中,我们计算了稀土过渡金属金属间化合物Sm(2)Fe(17)Z(3)(Z = C)的自旋和轨道矩,自旋和电荷密度以及4f晶体场(CF)参数,N)和Sm2Co17,采用相对论优化的原子轨道线性组合方法。迭代价电子态以局部自旋密度近似(LSDA)进行处理,而局部4f态被描述为经过自我相互作用校正的LSDA中的开核态。计算得出的磁矩与实验吻合良好。尽管Sm2Fe17的所有局部矩随晶格膨胀而增加,但与间隙位置相邻的原子的矩在插入间隙N或C后减小,而较远的Fe原子的矩在插入N或C时增加。在N间隙原子中,所有2p(α)轨道均与它们各自的Fe和Sm在键方向上邻近原子,而在C中,所有2p(α)轨道都与邻近间隙位置的Fe原子反平行地极化。发现控制稀土磁晶各向异性的二阶CF参数A(2)(0)具有与从磁化数据得出的符号和量级相同的符号和量级。根据实验,计算得出的Co化合物的负A(2)(0)大于Fe母体化合物,并且在插入间隙N或C时大大增加。在理论和实验之间的一致性通过考虑考虑到非4f态的交换相关电位的非球面性引起的CF贡献。 [参考:93]

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