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Correlation of electronic structure and ferromagnetism at rare earth metal surfaces.

机译:稀土金属表面的电子结构与铁磁性的相关性。

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摘要

The aim of this thesis is to understand surface magnetism from an electronic structure point of view. Specifically, heavy rare earth metal surfaces, especially Gd(0001) surface, were chosen because they provide the extreme examples of surface magnetism. Experimentally, spectroscopy techniques such as photoemission in different modes and spin-polarized photoemission, are utilized to probe the electronic structure and magnetic order of the bulk and surface.; A new surface state near E{dollar}sb{lcub}F{rcub}{dollar} in the vicinity of {dollar}barGamma{dollar} has been observed, which has 5d{dollar}sb{lcub}3zsp2-rsp2{rcub}{dollar} character and is spatially localized. Our experimental results and a recent theoretical calculation agree with each other on many aspects. The existence of this localized surface state explains the altered magnetic coupling and magnetic moment at the surface, and therefore provides considerable insight into the origin of that enhanced magnetic ordering at the Gd(0001) surface. This surface state is shown to be a magnetic state. There is an imperfect ferromagnetic coupling between the surface and bulk with a perpendicular component of magnetic moment at the surface.; Hydrogen dissociatively chemisorbs onto Gd(0001) surface to form 1 x 1 structure with no surface reconstruction observed. A pair of two-dimensional bands are induced by hydrogen adsorption. The highly localized 5d surface state of the clean surface is "converted" into a dispersive H-induced state. This "conversion" gives us the insight into the origin of the anticipated altered magnetic coupling and magnetic moment at the surface.; For the bulk bands, the exchange splitting changes with temperature while for the surface state, spin mixing is observed. A simple picture which embodies the differences in the relative localization is employed to understand these differences between the surface and the bulk.; The j-J coupling multiplet splittings of the 5p photoemission feature were observed and later calculated with an atomic calculation. The magnetic order is probed from the 5p levels with linearly polarized light. For paramagnetic rare earth metals {dollar}rm (T>Tsb{lcub}it c{rcub}){dollar} on a ferromagnetic substrate, magnetic order is induced in the overlayer, which can be modeled with Ginzberg-Landau's theory.
机译:本文的目的是从电子结构的角度理解表面磁。具体而言,选择重稀土金属表面,尤其是Gd(0001)表面,因为它们提供了表面磁性的极端示例。实验上,利用光谱技术,例如不同模式的光发射和自旋极化光发射,来探测块体和表面的电子结构和磁序。观察到在{dollar} barGamma {dollar}附近的E {dollar} sb {lcub} F {rcub} {dollar}附近有一个新的表面态,它具有5d {dollar} sb {lcub} 3zsp2-rsp2 {rcub } {dollar}字符,并且在空间上是局部的。我们的实验结果和最新的理论计算在许多方面都相互认可。这种局部表面状态的存在解释了表面处磁耦合和磁矩的变化,因此可以为Gd(0001)表面处增强的磁有序性的起源提供相当多的见识。该表面状态显示为磁性状态。在表面和主体之间存在不完善的铁磁耦合,并且在表面具有垂直的磁矩分量。氢解离地化学吸附到Gd(0001)表面上,形成1 x 1结构,没有观察到表面重建。氢吸附引起一对二维带。清洁表面的高度局部化的5d表面状态被“转换”为分散的H诱导状态。这种“转换”使我们深入了解了预期的表面磁耦合和磁矩改变的起源。对于主体带,交换分裂随温度而变化,而对于表面状态,观察到自旋混合。用一张体现相对定位差异的简单图片来理解表面和主体之间的这些差异。观察到5p光发射特征的j-J耦合多重分裂,随后通过原子计算进行计算。用线性偏振光从5p电平探测磁阶。对于铁磁衬底上的顺磁性稀土金属{rm}(T> Tsb {lcub} it c {rcub}),在覆盖层中感应出磁阶,可以用Ginzberg-Landau的理论进行建模。

著录项

  • 作者

    Li, Dongqi.;

  • 作者单位

    Syracuse University.;

  • 授予单位 Syracuse University.;
  • 学科 Physics Condensed Matter.; Engineering Materials Science.
  • 学位 Ph.D.
  • 年度 1993
  • 页码 147 p.
  • 总页数 147
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 工程材料学 ;
  • 关键词

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