cuboctahedra of the Au3Cu type. Er4Fe0.67Ga12 is iron-deficient, leading to a distortion of the octahedral and cuboctahedral environments due to the splitting of the Ga2 site into Ga2 and Ga3 sites. Further, interstitial octahedral sites that are unoccupied in Ln4FeGa12 (Ln = Y, Tb, Dy, and Ho) are partially occupied by Fe2. Y4FeGa12 exhibits weak itinerant ferromagnetism below 36 K. In contrast, Tb4FeGa12
LN 4 F
EGA 12,其中Ln为Y,Tb时,
镝,
钬,和Er,通过助熔剂生长制备,结晶与立方ÿ 4的PdGa 12结构与进出口3米的空间群,并用一个= 8.5650(4),8.5610 (4),8.5350(3),8.5080(3)和8.4760(3)Å。晶体结构由
铁镓八面体和面共享的Au 3 Cu型稀土立方八面体组成。尔4的Fe 0.67
镓12是缺
铁的,由于将Ga2位点分为Ga2和Ga3位点,导致八面体和立方八面体环境变形。此外,在Ln 4 F
EGa 12中未被占据的间隙八面体位点(Ln = Y,Tb,Dy和Ho)被Fe2部分占据。Y 4 F
EGa 12在36 K以下显示弱的迭代
铁磁。相反,Tb 4 F
EGa 12,Dy 4 F
EGa 12,Ho 4 F
EGa 12和Er 4 Fe 0.67 Ga 12在26、18.5、9和6 K时的摩尔磁化率具有最大的反
铁磁顺序。所有化合物均表现出
金属电阻率,在4