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Group-theoretical analysis of 1:3 A-site-ordered perovskite formation

机译:1:3 A-位序钙钛矿形成的群理论分析

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摘要

The quadruple perovskites AA′3 B 4 X 12 are characterized by an extremely wide variety of intriguing physical properties, which makes them attractive candidates for various applications. Using group-theoretical analysis, possible 1:3 A-site-ordered low-symmetry phases have been found. They can be formed from a parent perovskite structure (archetype) as a result of real or hypothetical (virtual) phase transitions due to different structural mechanisms (orderings and displacements of atoms, tilts of octahedra). For each type of low-symmetry phase, the full set of order parameters (proper and improper order parameters), the calculated structure, including the space group, the primitive cell multiplication, splitting of the Wyckoff positions and the structural formula were determined. All ordered phases were classified according to the irreducible representations of the space group of the parent phase (archetype) and systematized according to the types of structural mechanisms responsible for their formation. Special attention is paid to the structural mechanisms of formation of the low-symmetry phase of the compounds known from experimental data, such as: CaCu3Ti4O12, CaCu3Ga2Sn2O12, CaMn3Mn4O12, Ce1/2Cu3Ti4O12, LaMn3Mn4O12, BiMn3Mn4O12 and others. For the first time, the phenomenon of variability in the choice of the proper order parameters, which allows one to obtain the same structure by different group-theoretical paths, is established. This phenomenon emphasizes the fundamental importance of considering the full set of order parameters in describing phase transitions. Possible transition paths from the archetype with space group to all 1:3 A-site-ordered perovskites are illustrated using the Bärnighausen tree formalism. These results may be used to identify new phases and interpret experimental results, determine the structural mechanisms responsible for the formation of low-symmetry phases as well as to understand the structural genesis of the perovskite-like phases. The obtained non-model group-theoretical results in combination with crystal chemical data and first-principles calculations may be a starting point for the design of new functional materials with a perovskite structure.
机译:钙钛矿AA'3 B 4 X 12的四重特点是极具吸引力的物理特性,使其成为各种应用的有吸引力的候选材料。使用组理论分析,发现了可能的1:3 A位置排序的低对称相位。由于不同的结构机理(原子的有序和位移,八面体的倾斜),由于实际或假设的(虚拟)相变,它们可以由母钙钛矿结构(原型)形成。对于每种类型的低对称相位,确定了完整的顺序参数集(正确和不正确的顺序参数),计算的结构,包括空间组,原始单元乘法,Wyckoff位置的拆分以及结构公式。根据有序相的母体空间群(原型)的不可约表示对所有有序相进行分类,并根据负责其形成的结构机制的类型进行系统化。特别注意从实验数据中发现的化合物的低对称相的形成机理,例如:CaCu3Ti4O12,CaCu3Ga2Sn2O12,CaMn3Mn4O12,Ce1 / 2Cu3Ti4O 12 ,LaMn 3 Mn 4 O 12 ,BiMn 3 Mn 4 O 12 和别的。首次建立了在选择适当的阶数参数时会出现变化的现象,该现象使人们可以通过不同的组理论路径获得相同的结构。这种现象强调了在描述相变时考虑整套阶跃参数的根本重要性。使用Bärnighausen树形形式说明了从具有空间群的原型到所有1:3 A位置排序的钙钛矿的可能过渡路径。这些结果可用于识别新的相并解释实验结果,确定负责形成低对称相的结构机理,以及了解钙钛矿样相的结构成因。结合晶体化学数据和第一性原理计算获得的非模型群理论结果可能是设计具有钙钛矿结构的新型功能材料的起点。

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