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arXiv 1410.2802cond-mat.mtrl-sci
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巨磁热(Mn,Fe)2(P,Si,B)化合物铁磁相变的磁矩演化

Moment evolution across the ferromagnetic phase transition of giant magnetocaloric (Mn,Fe)2(P,Si,B) compounds

H. Yibole, F. Guillou, L. Caron, E. Jiménez, F. M. F. de Groot, P. Roy, R. de Groot, N. H. van Dijk, E. Brück

摘要:

一个强大的电子重建,导致淬火的Fe磁矩最近已被预测为在起源的巨磁热效应所显示的Fe 2 P基材料。为了验证这一假设,对(Mn,Fe)_2(P,Si,B)体系的两种典型组分在Mn和Fe的L边进行了X射线磁圆二色性实验。Mn和Fe的二向色吸收光谱在一级铁磁转变附近被测量为元素特异性的。实验光谱与第一原理计算和电荷转移多重态模拟进行比较,以获得磁矩。即使观察到的变磁性行为的签名作为温度或磁场的函数,Mn和Fe的磁矩演变的相似性表明,淬火的Fe时刻比以前预测的要弱。

英文摘要:

A strong electronic reconstruction resulting in a quenching of the Fe magnetic moments has recently been predicted to be at the origin of the giant magnetocaloric effect displayed by Fe2Pbased materials. To verify this scenario, X-ray Magnetic Circular Dichroism experiments have been carried out at the L edges of Mn and Fe for two typical compositions of the (Mn,Fe)2(P,Si,B) system. The dichroic absorption spectra of Mn and Fe have been measured element specific in the vicinity of the first-order ferromagnetic transition. The experimental spectra are compared with first-principle calculations and charge-transfer multiplet simulations in order to derive the magnetic moments. Even though signatures of a metamagnetic behaviour are observed either as a function of the temperature or the magnetic field, the similarity of the Mn and Fe moment evolution suggests that the quenching of the Fe moment is weaker than previously predicted.

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