Origin of magnetic anisotropy in R2Fe14B (R=rare earth) compounds: Crystalline electric field model calculations (abstract)

1987 ◽  
Vol 61 (8) ◽  
pp. 3472-3472
Author(s):  
S. K. Malik ◽  
E. B. Boltich ◽  
W. E. Wallace

The paramagnetic resonance spectra of five nickel Tutton salts have been analyzed at 290° K. The positions and intensities of the absorption lines are adequately explained by a crystalline electric field of rhombic symmetry. The triplet ground state is resolved into three singlets with an overall splitting of the order of 3 cm -1 , and the spectroscopic splitting factor g is found to be 2.25 ± 0.05. A comparison is made between the directly measured values of the magnetic anisotropy, and the values calculated using the resonance results.


1992 ◽  
Vol 115 (2-3) ◽  
pp. 281-286 ◽  
Author(s):  
Han Xiu-feng ◽  
Jin Han-min ◽  
Chen Hong ◽  
Guo Guang-hua ◽  
Zhao Tie-song

1965 ◽  
Vol 86 (6) ◽  
pp. 1235-1238 ◽  
Author(s):  
M N Ghatikar ◽  
A K Raychaudhuri ◽  
D K Ray

2017 ◽  
Vol 19 (20) ◽  
pp. 13245-13251 ◽  
Author(s):  
Kai-Cheng Zhang ◽  
Yong-Feng Li ◽  
Yong Liu ◽  
Yan Zhu ◽  
Li-Bin Shi

The rare-earth dimers adsorbed onto graphene oxide possess huge magnetic anisotropy which can be effectively tuned by electric field.


The theory that has been developed for rare-earth ions in crystals is here applied to the double nitrates. The paramagnetic resonance data and certain spectroscopic properties of the different rare-earth double nitrates, depending as they do on the crystalline electric field at a rare-earth ion, are related to the six parameters through which the field is defined. It is found that most of the experimental results can be fitted to values of the parameters that vary in a systematic fashion along the rare-earth series.


1996 ◽  
Vol 10 (29) ◽  
pp. 1471-1476
Author(s):  
MIRCEA ANDRECUT

The temperature dependence of the second-order crystalline electric field (CEF) parameters of rare earth intermetallic compound CeZn 2 was deduced from the least-squares nonlinear fit to the reciprocal paramagnetic susceptibility along principal crystalline axes. The results of the calculation are in good agreement with the experimental values.


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