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首页> 外文期刊>THE CANADIAN MINERALOGIST >PARAMETERIZATION OF CENTROSYMMETRIC ELPASOLITE-TYPE CRYSTAL STRUCTURES IN TERMS OF SYMMETRY-ADAPTED BASIS-VECTORS OF THE PRIMITIVE CUBIC ARISTOTYPE PHASE
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PARAMETERIZATION OF CENTROSYMMETRIC ELPASOLITE-TYPE CRYSTAL STRUCTURES IN TERMS OF SYMMETRY-ADAPTED BASIS-VECTORS OF THE PRIMITIVE CUBIC ARISTOTYPE PHASE

机译:本构相适应的基体ASUtotype阶段术语中的对称心形锂电晶体结构的参数化

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摘要

Group-theory methods are used to decompose the crystal structures of centrosymmetric double perovskites, A_2BB'X_6, that exhibit zone-boundary tilting of octahedra and the rock-salt pattern of order of the B-site cations, typified by the mineral elpasolite, K_2NaAlF_6. For the twelve space-groups consistent with these phenomena, the associated structures are decomposed in terms of the magnitudes of an appropriate set of symmetry-adapted basis-vectors of the primitive cubic aristotype phase of perovskite at high-symmetry points of the Brillouin zone. The method is outlined using the example of Sr_2YNbO_6 in space group P2_1; full results that can be utilized in the decomposition of the other space-groups are tabulated. The advantages of decomposing elpasolite-structured phases in this way are further illustrated using the temperature dependence of the crystal structure of Ba_2SbBiO_6 between 4.2 and 625 K.
机译:使用群论方法分解中心对称双钙钛矿A_2BB'X_6的晶体结构,该晶体结构显示八面体的区域边界倾斜和B位阳离子阶次的岩盐模式,其特征为矿物锂辉石K_2NaAlF_6 。对于与这些现象相一致的十二个空间群,在布里渊区的高对称点处,钙钛矿原始立方贵族相的一组适当的对称适应基矢量的大小,将相关结构分解。使用空间组P2_1 / n中的Sr_2YNbO_6的示例概述了该方法;列出了可用于分解其他空间组的全部结果。使用Ba_2SbBiO_6的晶体结构在4.2到625 K之间的温度依赖性,可以进一步说明以这种方式分解钙钛矿结构相的优势。

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