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Crystal structure and magnetic properties of the UFe7Al5 uranium-iron aluminide

机译:UFe7Al5铀铁铝化物的晶体结构和磁性

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The ternary compound UFe7Al5 was synthesized by arc melting, followed by annealing at 850degreesC. The crystal structure was determined by single-crystal X-ray diffraction and refined to a residual value of R = 0.039 (S = 1.030), with lattice parameters a = 8.581(2) Angstrom and c = 4.946(l) Angstrom. This compound is a new extreme composition in the family of intermetallics with general formula UFexAl12-x crystallizing in the tetragonal ThMn12-type structure, space group I4/mmm. In contrast to UFexAl12-x within the composition range 4 less than or equal to x less than or equal to 6, in UFe7Al5 the additional iron atom is found in the 8i equipositions. Magnetization measurements versus temperature show two magnetic transitions at 363 and 275 K, respectively, with a ferromagnetic behavior below the highest temperature transition. Fe-57 Mossbauer data indicate that the high-temperature transition is related to the ordering of the iron atoms. The dependence of the isomer shifts and magnetic hyperfine fields on the crystallographic site and on the number of the iron nearest neighbors is similar to that observed in the other UFexAl12-x and rare-earth analogues. The magnetic hyperfine field values of iron atoms on 8i sites is larger than in the other sites, in agreement with previous data obtained for other ThMn12-type compounds. (C) 2003 Elsevier Inc. All rights reserved. [References: 32]
机译:通过电弧熔化,然后在850℃下退火,合成三元化合物UFe7Al5。通过单晶X射线衍射确定晶体结构,并将其精炼至R = 0.039(S = 1.030)的残余值,其晶格参数a = 8.581(2)埃,c = 4.946(1)埃。该化合物是金属间化合物家族中的一种新的极端组成,其通式为UFexAl12-x结晶为四方ThMn12型结构,空间群为I4 / mmm。与组成范围4小于或等于x小于或等于6的UFexAl12-x相反,在UFe7Al5中,在8i等位物中发现了额外的铁原子。磁化强度与温度的关系曲线分别显示了在363 K和275 K处的两个磁跃迁,其铁磁行为低于最高温度跃迁。 Fe-57 Mossbauer数据表明高温转变与铁原子的有序化有关。异构体位移和磁场超精细场对晶体学位点和最邻近的铁原子数的依赖性类似于在其他UFexAl12-x和稀土类似物中观察到的依赖性。与其他ThMn12型化合物获得的先前数据相一致,在8i位点上铁原子的超磁场磁场值大于其他位点。 (C)2003 Elsevier Inc.保留所有权利。 [参考:32]

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