斯库特绿铁矿
核四极共振
金属-绝缘体过渡
凝聚态物理
三角晶系
材料科学
空间组
四极
金属
共振(粒子物理)
过渡金属
结晶学
对称(几何)
核磁共振
物理
晶体结构
原子物理学
化学
X射线晶体学
光学
热电材料
生物化学
冶金
催化作用
数学
复合材料
热导率
几何学
衍射
作者
Satoru Masaki,T. Mito,Masayuki Takemura,Shinji Wada,Hisatomo Harima,Daisuke Kikuchi,Hideyuki Sato,Hitoshi Sugawara,N. Takeda,Guo‐qing Zheng
标识
DOI:10.1143/jpsj.76.043714
摘要
We report the results of NQR (nuclear quadrupole resonance) study on SmRu 4 P 12 , one of a few candidates for materials showing octupolar ordering. In this study, we firstly succeeded in observing the 101 Ru-NQR signal in filled skutterudite compounds R Ru 4 P 12 ( R : rare earth). A single 101 Ru-NQR signal splits into two resonance lines, having intensity ratio of 3:1, just below the metal–insulator ( M – I ) transition temperature of 16.5 K. This result gives convincing evidence for symmetry lowering in the ordered state of this compound, namely the cubic I m \bar3 space group for the filled skutterudite compounds is lowered to the trigonal R \bar3. The model of the ordered structure characterized by a wave vector q =(1,0,0) satisfactorily explains the observed phenomena in the present study and the M – I transition in this compound.
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