Structure and ferromagnetism of the rare-earth zintl compounds:: Yb14MnSb11 and Yb14MnBi11

Structure and ferromagnetism of the rare-earth zintl compounds:: Yb14MnSb11 and Yb14MnBi11
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DOI:
10.1021/cm980358i
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发表时间:
1998-11-01
影响因子:
8.6
通讯作者:
Webb, DJ
Webb, DJ
中科院分区:
材料科学2区
文献类型:
--
作者:
Chan, JY;Olmstead, MM;Webb, DJ

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稀土过渡金属化合物Yb 14 MnSb 11和Yb 14 MnBi 11是通过在1000-1200 ℃加热化学计量量的元素制备的。这些化合物与Zintl化合物Ca_(14)AlSb_(11)是同构的,并且在四元空间群I_4(1)/acd(Z = 8)中结晶。对Yb 14 MnSb 11的单晶X射线数据(143 K)进行了修正[a = 16.615(2)Angstrom,c = 21.948(4)Angstrom,V = 6059(2)Angstrom(3),R1/wR 2(0.0299/0.0479)]和Yb 14 MnBi 11 [α = 17.000(3)埃,22.259(6)埃,V = 6433(2)埃(3),R1/wR 2(0.0631/0.133)]。结构分析与Yb 2+一致。随温度变化的磁化率数据表明,Yb 14 MnSb 11在56 K时为铁磁有序,而Yb 14 MnBi 11在58 K时发生铁磁转变,在28 K时又发生铁磁转变.高温磁化率数据可用修正的Curie-Weiss定律拟合,Sb和Bi化合物的μ(eff)= 4.92(2)μ(B)和μ(eff)= 4.9(1)μ(B)。这一结果与Mn ~(3+)(d(4))和Yb ~(2+)(f(14))的归属一致。单晶的磁性数据提供了额外的证据的磁性转变,并表明该化合物是磁各向异性。
Rare-earth transition metal compounds Yb14MnSb11 and Yb14MnBi11 have been prepared by heating stoichiometric amounts of the elements at 1000-1200 degrees C. These compounds are isostructural with the Zintl compound Ca14AlSb11 and crystallize in the tetragonal space group I4(1)/acd (Z = 8). Single-crystal X-ray data (143 K) were refined for Yb14MnSb11 [a = 16.615(2) Angstrom, c = 21.948(4) Angstrom, V = 6059(2) Angstrom(3), and R1/wR2 (0.0299/0.0479)] and Yb14MnBi11 [a = 17.000(3) Angstrom, 22.259(6) Angstrom, V = 6433(2) Angstrom(3), R1/wR2 (0.0631/0.133)]. Structural analysis is consistent with Yb2+. Temperature-dependent magnetic susceptibility data show that Yb14MnSb11 orders ferromagnetically at 56 K and Yb14MnBi11 has a ferromagnetic transition at 58 K and another transition at 28 K. High-temperature magnetic susceptibility data can be fit with a modified Curie-Weiss law and give mu(eff) = 4.92(2)mu(B) and mu(eff) = 4.9(1)mu(B) for the Sb and Bi compounds, respectively. This result is consistent with the assignment of Mn3+ (d(4)) and Yb2+ (f(14)). Single-crystal magnetic data provide additional evidence for the magnetic transitions and show that the compounds are magnetically anisotropic.