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Transferred hyperfine interaction between the rare-earth ions and the fluorine nuclei in rare-earth trifluorides

机译:稀土离子与稀土三氟化物中的氟原子核之间转移的超精细相互作用

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摘要

The isotropic and anisotropic transferred hyperfine interactions between F ions in the two chemically inequivalent sites and the rare-earth ions (R) have been derived from 19F NMR measurements in the temperature region 100-300 K on single crystals of TbF3 and DyF3. The isotropic interactions are found to be negative and constant in this temperature region and with the numerical values decreasing slightly from TbF3 to DyF3. The anisotropic interactions, when the point dipole contributions are subtracted, are found to be substantially smaller and about equal for the two materials. The crystals contain two symmetry related magnetic sublattices A and B, contributing to the macroscopic susceptibility. The sublattice susceptibility has an off-diagonal component χacA and χacB=-χacA in the crystalline axes system. The orientations of the principal axes of the two subattice susceptibilities are found to vary only slightly with temperature. They are further assigned to definite R's in the unit cell, which cannot be done from macroscopic magnetic measurements.
机译:两个化学不等价位点中的F离子与稀土离子(R)之间的各向同性和各向异性转移的超精细相互作用是根据TbF3和DyF3单晶在100-300 K温度范围内的19F NMR测量得出的。发现各向同性相互作用在此温度范围内为负且恒定,数值从TbF3到DyF3略有降低。当减去点偶极子贡献时,发现两种材料的各向异性相互作用基本上较小并且大约相等。晶体包含两个对称的相关磁亚晶格A和B,有助于形成宏观磁化率。亚晶格磁化率在晶轴系统中具有非对角线分量χacA和χacB=-χacA。发现两个亚晶格磁化率的主轴方向仅随温度变化。它们还被分配给单位晶格中的确定R,这是无法通过宏观磁测量完成的。

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