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Magnetic properties of the iron sublattice in the YFe12xMx compounds (M = Ti, Mo or V; x = 1–3.5)

机译:YFe12xMx化合物中铁亚晶格的磁性(M = Ti,Mo或V; x = 1-3.5)

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The magnetic properties of the YFe12xMx compounds (M = Ti, Mo or V; x = 1–3.5) have been determined in the orde red ferromagnetic state as well as in the paramagnetic state. The iron magnetic moment has been determined from 4 K up to the Curie temperature whereas the analysis of the paramagnetic region has led to the determination of the effective iron magnetic moment. The number of spins has been calculated below and above the Curie temperature in order to discuss the degree of itinerancy of the Fe magnetic behavior in the YFe12xMx compounds. All the YFe12xMx compounds (M = Ti, Mo or V; x = 1–3.5) have very similar crystalline properties: they crystallize in the same crystal structure and all the M elements used here are known to substitute for iron on the same crystal site. In contrast, they exhibit a wide range of magnetic behavior; the Curie temperature varies from 63 to 539 K and the mean magnetic moment per iron atom is also very dependent upon the M element used and its concentration. Furthermore the degree of itinerancy of the iron is not preserved along YFe12xMx compounds but is found to depend significantly upon the nature of the substituting element M and its concentration. The results are discussed and compared to earlier published results obtained on binary R–Fe and ternary R–Fe–B compounds.
机译:YFe12xMx化合物(M = Ti,Mo或V; x = 1-3.5)的磁性已在红色铁磁状态和顺磁性状态下确定。已经确定了从4 K到居里温度的铁磁矩,而对顺磁区域的分析导致了有效铁磁矩的确定。为了讨论YFe12xMx化合物中Fe磁行为的迭代程度,已经计算了居里温度以下和以上的自旋数。所有YFe12xMx化合物(M = Ti,Mo或V; x = 1–3.5)具有非常相似的结晶特性:它们以相同的晶体结构结晶,并且此处使用的所有M元素都可以替代相同晶体上的铁。 。相反,它们表现出广泛的磁性。居里温度在63至539 K之间变化,每个铁原子的平均磁矩也非常取决于所用M元素及其浓度。此外,沿YFe12xMx化合物不保留铁的迭代度,但发现其很大程度上取决于取代元素M的性质及其浓度。对结果进行了讨论,并将其与较早发表的有关二元R–Fe和三元R–Fe–B化合物的结果进行了比较。

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