取代效应对一些类似钙钛矿的高级功能材料的轨道有序性和多铁性

K. Krezhov
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摘要

替代是设计具有钙钛矿结构的新型功能材料的一种可行手段。钙钛矿结构的A位和B位都会受到影响。我们表明,磁性相互作用和其他重要材料的电子性质,如巨磁阻(CMR)六方双钙钛矿和锰酸盐,或多铁性RMn2O5 (R=稀土金属)可能会受到影响,但要理解为什么化合物没有显示预期的性质,需要在微观水平上的详细信息。事实上,与典型的CMR化合物Sr2FeMoO6(铁磁性和半金属)不同,Ba2MSbO6 (M=Fe, Co)由于明显的反位无序而缺乏长程磁有序和自旋玻璃行为。母电荷中有序bi0.5 a0.5 femn1 - xo3 (A=Ca, Sr)用Fe3+取代Mn3+破坏了已知的阻碍CMR行为的电荷顺序,而不会引起磁阻效应。同样,虽然Mn的部分取代似乎是增加多铁性YbFeMnO5中磁化和电极化之间交联的方式,但我们发现它在YbFeMnO5结构中的两个过渡金属位置之间引入了低水平的无序性。缺乏晶体相变到极空间群的证据排除了自发电极化的期望。此外,当k = 0时,观察到的共线磁性结构不允许自旋极化,因此,YbMnFeO5不被认为是多铁化合物。
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Substitution effects on orbital ordering and multiferroicity in some perovskite-like candidates for advanced functional materials
Substitution is a feasible means in designing novel functional materials with perovskite-like structure. Both A- and B- sites of the perovskite structure could be affected. We show that the magnetic interactions and other electronic properties of important materials such as colossal magnetoresistive (CMR) hexagonal double perovskites and manganates, or multiferroic RMn2O5 (R=rare earth metal) could be influenced but to understand why the compound does not display the expected properties calls for detailed information on microscopic level. Indeed, unlike ferromagnetic and half metallic Sr2FeMoO6, which is a paradigmatic CMR compound, lack of long-range magnetic ordering and spin glass behavior was established in Ba2MSbO6 (M=Fe, Co) due to a significant antisite disorder. In the parent charge ordered Bi0.5A0.5FexMn1-xO3 (A=Ca, Sr) substitution with Fe3+ for Mn3+ destroyed the charge order known to hamper CMR behavior without to induce magnetoresistive effect. Similarly, although partial substitution of Mn seems to be the way to increase the crosslink between magnetization and electric polarization in multiferroic YbMn2O5 we found that it introduces a low level of disorder between the two transition metal positions in the YbFeMnO5 structure. The lack of evidence for a crystallographic phase transition to a polar space group rules out expectations of a spontaneous electric polarization. In addition, the observed collinear magnetic structure with k = 0 does not permit a spin polarization and, therefore, YbMnFeO5 is not expected to be a multiferroic compound.
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