^<31>P Nuclear magnetic resonance and ^<101>Ru nuclear quadrupole resonance measurements of filled skutterudites GdRu_4P_<12> and TbRu_4P_<12>
^<31>P Nuclear magnetic resonance and ^<101>Ru nuclear quadrupole resonance measurements of filled skutterudites GdRu_4P_<12> and TbRu_4P_<12>
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^<31>P 填充方钴矿 GdRu_4P_<12> 和 TbRu_4P_<12> 的核磁共振和 ^<101>Ru 核四极共振测量
DOI:
10.1143/jpsj.80.044713
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发表时间:
2011
期刊:
影响因子:
--
通讯作者:
H.Fukazawa
中科院分区:
文献类型:
--
作者:
K.Someya;A.Bamba;M.Ishida;H.Fukazawa
Filled skutterudites GdRu4P12and TbRu4P12exhibit antiferromagnetic ordering below 22 and 20 K, respectively. In TbRu4P12, an additional anomaly exists at around 10 K under a zero field; the origin of this successive transition might be related to multipole ordering. In order to determine the detailed magnetic properties of GdRu4P12and TbRu4P12, we performed zero-field31P nuclear magnetic resonance (NMR) and101Ru nuclear quadrupole resonance (NQR) measurements on them. The zero-field31P-NMR spectra indicate the occurrence of magnetic transition only at 22 K (GdRu4P12) and 20 K (TbRu4P12). We observed an anomalous temperature dependence of the spin–lattice relaxation rate 1/T1just below 20 K and a small anomaly at around 10 K in the101Ru-NQR of TbRu4P12. The temperature dependence of 1/T1also indicates that the nesting condition in the ordered states of GdRu4P12and TbRu4P12is poorer than that of SmRu4P12.