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Interplay among spin, charge and the lattice in perovskite manganites.

机译:钙钛矿锰矿中自旋,电荷和晶格之间的相互作用。

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摘要

Perovskite manganites have received much attention due to the large magnetoresistance observed near the Curie Temperature {dollar}Tsb{lcub}C{rcub},{dollar} which marks the transition from a high-temperature paramagnetic insulator to a low-temperature ferromagnetic metal. We have studied 30% hole-doped LaMnO{dollar}sb3,{dollar} the doping range for optimal ferromagnetism, and found a rich phase diagram as a function of the average ionic radius of the La-site {dollar}langle rsb{lcub}A{rcub}rangle,{dollar} which is varied by substituting different rare earth ions for La. With decreasing {dollar}langle rsb{lcub}A{rcub}rangle, Tsb{lcub}C{rcub}{dollar} decreases rapidly and the magnitude of the magnetoresistance increases exponentially, until a zero temperature insulating phase is entered.; The structure of this phase diagram is consistent with changes is the electronic bandwidth induced by changes in the Mn-O bond lengths and the Mn-O-Mn bond angles, as measured by neutron diffraction. We find that the effects of applied pressure can be mapped onto changes in {dollar}langle rsb{lcub}A{rcub}rangle,{dollar} which can be thought of as a form of internal "chemical" pressure. In addition to structurally induced changes in the bandwidth, we demonstrate the important role of distortions of the MnO{dollar}sb6{dollar} octahedra, which increase with decreasing {dollar}langle rsb{lcub}A{rcub}rangle,{dollar} providing a tendency towards charge localization.; We have also examined the magnetoresistance in the low temperature ferromagnetic metallic state of single crystal and polycrystalline {dollar}rm Lasb{lcub}2/3{rcub}Srsb{lcub}1/3{rcub}MnOsb3.{dollar} We find that the intrinsic negative magnetoresistance in single crystal is due to the suppression of spin fluctuations, and magnetic domain boundaries do not dominate the scattering process. In contrast, in polycrystalline samples we find a large low-field magnetoresistance dominated by spin-polarized tunneling between grains.; Finally we present inelastic neutron scattering experiments on the spin dynamics in {dollar}rm Prsb{lcub}0.63{rcub}Srsb{lcub}0.37{rcub}MnOsb3.{dollar} Two distinct new features have been observed: a softening of the magnon dispersion at the zone boundary for {dollar}T
机译:由于在居里温度Tsb {lcub} C {rcub}附近观察到较大的磁阻,钙钛矿锰矿受到了广泛的关注,这标志着从高温顺磁绝缘体到低温铁磁金属的转变。我们研究了30%的空穴掺杂LaMnO {dollar} sb3,{dollar}以获得最佳铁磁性的掺杂范围,并发现了丰富的相图,该相图是La位置{dolal} langle rsb {lcub的平均离子半径的函数} A {rcub} rangle,{dollar}通过用不同的稀土离子替代La而变化。随着{dollar} langle rsb {lcub} A {rcub} r的减小,Tsb {lcub} C {rcub} {dollar}减小迅速,并且磁阻的大小呈指数增加,直到进入零温度绝缘阶段为止。该相图的结构与变化是一致的,即通过中子衍射测量的Mn-O键长和Mn-O-Mn键角的变化所引起的电子带宽。我们发现,施加压力的影响可以映射到{dollar} rsb {lcub} A {rcub} rangle {dollar}中的变化,这可以认为是内部“化学”压力的一种形式。除了结构上引起的带宽变化外,我们还证明了MnO {dollar} sb6 {dollar}八面体的畸变的重要作用,该畸变随{dollar} lrsb {lcub} A {rcub} rangle {{dollar}提供电荷本地化的趋势。我们还研究了单晶和多晶{dol} rm Lasb {lcub} 2/3 {rcub} Srsb {lcub} 1/3 {rcub} MnOsb3的低温铁磁金属态的磁阻。{dollar}单晶中的固有负磁阻是由于自旋波动的抑制,并且磁畴边界并不主导散射过程。相反,在多晶样品中,我们发现了一个大的低场磁阻,主要由晶粒之间的自旋极化隧穿构成。最后,我们对{rm} rm Prsb {lcub} 0.63 {rcub} Srsb {lcub} 0.37 {rcub} MnOsb3的自旋动力学进行了非弹性中子散射实验。观察到两个明显的新特征:磁振子的软化{美元} T

著录项

  • 作者

    Hwang, Harold Yoonsung.;

  • 作者单位

    Princeton University.;

  • 授予单位 Princeton University.;
  • 学科 Physics Condensed Matter.; Engineering Materials Science.
  • 学位 Ph.D.
  • 年度 1997
  • 页码 103 p.
  • 总页数 103
  • 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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