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Magnetostriction in mixed valent magnetic oxides

机译:混合价磁氧化物中的磁致伸缩

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Since the early discovery of the magnetostriction effects on iron by Joule and the Invar alloys by Ch. E. Guillaume, a vast discipline emerged in solid state physics. From the basic point of view based on thermodynamic and symmetry considerations, the first phenomenological explanation of the magnetostriction was established by Becker R., Doring W. (1939), Lee E. W. (1955). An important contribution to the explanation of the magnetostriction incorporating a Quantum-Mechanics formalism is due to Callen E. R. & Callen H. B. (1963) who really established the grounds of the modern magnetostriction theory for localised magnetic moment systems. In a broad sense, it is considered that magnetostriction has as origin the spin-orbit coupling, which is manifested in two different kinds of magnetostriction behaviours. One is isotropic, giving rise to volume effects, and the other of anisotropic nature, having its origin in a local distortion of the lattice, due to a preferential orientation of the angular moment of the magnetic electronic charge cloud. Those mechanisms are well explained in systems with localised magnetic moments. Good examples of this effect are observed in rare earth metals, and their alloys, mainly with 3d metals (Fe, Co, Ni), in the Laves phase structure (RM{sub}2) and also in cubic RZn. The largest room temperature effect was found in Terfenol (Th-Dy) Fe{sub}2 alloy, which is the base of the commercial materials for magnetostrictive applications. In these systems, the isotropic effect, i.e. volume magnetostriction, is small and originated either by field induced change of the intrinsic magnetisation (paraprocess), giving rise to the forced magnetostriction, or by the change with the distance of the exchange interaction between localised magnetic moments.
机译:自焦耳和CH的Invar合金的早期发现磁致伸缩作用。 E. Guillaume,一个在固态物理学中出现的巨大纪律。从基于热力学和对称考虑的基本观点来看,磁致伸缩的第一个现象学解释由Becker R.,Doring W.(1939),Lee E. W.(1955)。对包含量子力学形式主义的磁致伸缩的解释的重要贡献是由于Callen E. R.&Callen H. B.(1963)真正建立了局部磁矩系统的现代磁致伸缩理论的理由。在广泛的意义上,认为磁致伸缩具有起始旋转轨道耦合,其在两种不同种类的磁致索行为中表现出来。一种是各向同性的,引起体积效应,以及另一个各向异性性质,其原点在晶格的局部变形中,由于磁电子荷云的角矩的优先取向。这些机制在具有局部磁矩的系统中得到了很好的解释。在稀土金属及其合金中观察到这种效果的良好实例,主要是在Laves相位结构(RM {Sub} 2)中以及三次RZN中的3D金属(Fe,Co,Ni)。在Terfenol(Th-Dy)Fe {Sub} 2合金中发现了最大的室温效果,这是磁致伸缩应用的商业材料的基础。在这些系统中,通过现场磁化(Paraprocess)的现场诱导变化的各向同性效应,即体积磁致伸缩,从而产生强制磁致伸缩,或通过局部磁性之间的交换相互作用的距离变化,或者通过局部磁性之间的交换相互作用的变化来起源时刻。

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