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arXiv 1502.07510cond-mat.str-el
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基于从头计算的W(110)和Ta(110)表面Fe单层的磁性phase diagram

Magnetic phase diagram of an Fe monolayer on W(110) and Ta(110) surfaces based on ab initio calculations

Levente Rózsa, László Udvardi, László Szunyogh, István A. Szabó

摘要:

本文基于从头算屏蔽的Korringa-Kohn-Rostoker方法,对W和Ta(110)表面上Fe单层膜的磁性进行了详细的研究。通过计算张量交换耦合系数,利用原子自旋动力学模拟确定了系统的基态。不同类型的基态被发现在系统中作为Fe层的弛豫的函数。在W(110)衬底的情况下,这反映在易轴从面内到面外的重新取向中。对于Ta(110),出现了从铁磁态到摆线自旋螺旋态,然后到另一个波矢较大的自旋螺旋态的转变,并且在大弛豫时,发现自旋螺旋的法向矢量发生了旋转.经典的蒙特卡罗模拟表明,在Fe/Ta(110)系统中观察到的不同磁相之间存在温度诱导的转变.这些相变进行了定量和定性分析的有限温度自旋波理论。

英文摘要:

We present detailed investigations of the magnetic properties of an Fe monolayer on W and Ta (110) surfaces based on the ab initio screened Korringa-Kohn-Rostoker method. By calculating tensorial exchange coupling coefficients, the ground states of the systems are determined using atomistic spin dynamics simulations. Different types of ground states are found in the systems as a function of relaxation of the Fe layer. In case of W(110) substrate this is reflected in a reorientation of the easy axis from in-plane to out-of-plane. For Ta(110) a switching appears from the ferromagnetic state to a cycloidal spin spiral state, then to another spin spiral state with a larger wave vector and, for large relaxations, a rotation of the normal vector of the spin spiral is found. Classical Monte Carlo simulations indicate temperature-induced transitions between the different magnetic phases observed in the Fe/Ta(110) system. These phase transitions are analyzed both quantitatively and qualitatively by finite-temperature spin wave theory.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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