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Magnetic susceptibility of the rare earth phosphomolybdates.

机译:稀土磷钼酸盐的磁化率。

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The most recent work on the magnetic susceptibility of rare earth phosphomolybdates, RPO4(MoO3)12·30H 2O (or RPMO) is described here. R denotes the trivalent ions Ce, Pr, Nd, Gd, Tb, Dy, Ho, Er, Tm, or Yb. Some data on iron phosphomolybdate (FePMO) and chromium phosphomolybdate (CrPMO) is also included. The paramagnetic susceptibilities of FePMO, CrPMO and GdPMO are Curie-Weiss like from 300 K to 0.1K. The paramagnetic susceptibility data from 300 K to 0.1 K of the other RPMO salts was compared to theoretical curves based on the assumption that the magnetic ions have 23 (T) site symmetry. There was good agreement between these curve fits and the susceptibility data of DyPMO, ErPMO, and YbPMO. TbPMO and HoPMO have magnetic ground states due to mixing caused by the nuclear hyperfine interaction and the data of HoPMO, in particular, could be fit reasonably well once the hyperfine interaction was included in the curves. The hyperfine interaction seems to be weak in TmPMO. The susceptibility of the lighter RPMO could not be fit with curves based on the assumption that the magnetic ions have 23 (T) site symmetry. Magnetic ordering was observed in FePMO, GdPMO, DyPMO, ErPMO and YbPMO. There may be some exchange magnetism in FePMO but GdPMO, DyPMO, ErPMO and YbPMO are likely to be dipolar magnets. If these salts have the Fd3¯ ( T4h ) space symmetry above the ordering temperature then a classical dipolar calculation predicts that a monoclinic PBb(Cc) magnetic structure has the lowest energy. The susceptibilities of FePMO, DyPMO, ErPMO and YbPMO near absolute zero are equal to or less than that predicted for a classical PBb(PCc) dipolar magnet. A "diamond" like spin wave calculation shows some qualitative agreement with these susceptibilities. The susceptibility of GdPMO is much higher than that of a classical P Bb(PCc) magnet.
机译:此处介绍了稀土磷钼酸盐RPO4(MoO3)12·30H 2O(或RPMO)的磁化率的最新工作。 R表示三价离子Ce,Pr,Nd,Gd,Tb,Dy,Ho,Er,Tm或Yb。还包括有关磷钼酸铁(FePMO)和磷钼酸铬(CrPMO)的一些数据。 FePMO,CrPMO和GdPMO的顺磁化率从300 K到0.1K为居里-魏斯。基于磁性离子具有23(T)位对称性的假设,将其他RPMO盐的300 K至0.1 K的顺磁化率数据与理论曲线进行了比较。这些曲线拟合与DyPMO,ErPMO和YbPMO的磁化率数据之间有很好的一致性。由于核超精细相互作用引起的混合,TbPMO和HoPMO具有磁性基态,特别是一旦曲线中包含超精细相互作用,HoPMO的数据就可以很好地拟合。 TmPMO中的超精细相互作用似乎很弱。基于磁性离子具有23(T)位置对称性的假设,较轻的RPMO的磁化率无法与曲线拟合。在FePMO,GdPMO,DyPMO,ErPMO和YbPMO中观察到磁性排序。 FePMO中可能存在一些交换磁性,但GdPMO,DyPMO,ErPMO和YbPMO可能是偶极磁体。如果这些盐在有序温度以上具有Fd3(T4h)空间对称性,则经典的偶极计算预测单斜PBb(Cc)磁性结构的能量最低。 FePMO,DyPMO,ErPMO和YbPMO的磁化率接近绝对零,等于或小于经典PBb(PCc)双极磁体的磁化率。像自旋波计算这样的“钻石”显示出与这些磁化率的定性一致性。 GdPMO的磁化率远高于传统的P Bb(PCc)磁体。

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