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The susceptibilities and molecular-field constants of rare-earth compounds from mean-field theory

机译:基于平均场理论的稀土化合物的磁化率和分子场常数

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The mean-field theory is employed in present work to study the validity conditions for a popular formula which is widely used to calculate the susceptibilities of rare-earth compounds and their molecular-field constants from known transition temperatures [Proc. R. Soc. Lond. 276A (1963) 19; Phys. Rev. 163 (1967) 444]. To facilitate the theoretical analysis, we consider a special system, CeTe_2, whose magnetic behavior below T_N is mainly governed by the lowest crystal-field (CF) Kramers doublet according to our recent theoretical studies. We find that, when the external field and the localized moment are both considerably weak, the formula can be safely used, but, when their magnitudes are appreciable with respect to temperature, one has to include the both terms in the Hamiltonian and perform the calculations self-consistently in order to calculate the susceptibility accurately; and to reflect the intrinsic magnetic properties of a system, the external field must be very weak in experimental measurements or theoretical calculations. Finally, we propose an alternative approach to determine the exchange constant from the known transition temperature, or vice versa.
机译:在目前的工作中,采用均值场理论来研究一个流行公式的有效性条件,该公式被广泛用于从已知的转变温度计算稀土化合物的磁化率及其分子场常数。 R. Soc。 nd 276A(1963)19;物理Rev. 163(1967)444]。为了便于理论分析,我们考虑一种特殊的系统CeTe_2,根据我们最近的理论研究,该系统的磁行为在T_N以下主要受最低晶体场(CF)Kramers doublet控制。我们发现,当外场和局域矩都相当弱时,可以安全地使用该公式,但是,当它们的幅度相对于温度可观时,则必须将这两项都包含在哈密顿量中并进行计算自洽以准确计算磁化率;为了反映系统的固有磁性能,在实验测量或理论计算中,外部磁场必须非常弱。最后,我们提出了另一种方法,可从已知的转变温度确定交换常数,反之亦然。

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