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A First Order Phase Transition and Self-organizing States in Single-domain Ferromagnet

机译:单畴铁磁体中的一阶相变和自组织态

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Analytical consideration of uni-axial single-domain ferromagnet during the first order phase transition induced by a magnetic field is performed. Field is directed along the symmetry axis antiparallel to initial magnetization direction. For samples of the flat shape, besides the known change of the magnetization direction on 180o, at definite relations between values of magnetic field, the magnetization and the anisotropy of a crystall, there is continuous spectrum of states with intermediate magnetization directions. In these states, a precession frequency ω = 0. For samples of spherical shape, a process of the phase transition does not depend on the demagnetization field. At addition action of high frequency field perpendicular to the main magnetic field, there are dynamic equilibrium states, i.e. "self-organizing states" of ferromagnet, when the entropy increase connected with dissipation is compensated by the negative entropy flow due to the periodic field. It is shown that under these conditions, by varying the frequency of the periodic field, we can control the self-organising system, i.e. decrease or increase the system energy and, correspondingly, change the direction of magnetisation in ferromagnet.
机译:对磁场引起的一阶相变过程中的单轴单畴铁磁体进行了分析考虑。磁场沿着对称轴反平行于初始磁化方向。对于扁平状的样品,除了已知的180o磁化方向变化外,在磁场值,磁化强度和晶体各向异性之间存在明确的关系时,存在具有中间磁化方向的连续光谱。在这些状态下,进动频率ω=0。对于球形样品,相变过程不依赖于退磁场。在垂直于主磁场的高频场的加法作用下,存在动态平衡状态,即铁磁体的“自组织状态”,这是由于周期性磁场引起的负熵流补偿了与耗散有关的熵增加。结果表明,在这些条件下,通过改变周期磁场的频率,我们可以控制自组织系统,即减少或增加系统能量,并相应地改变铁磁体的磁化方向。

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