首页> 外文期刊>International Journal of Quantum Chemistry >Crystal structure, stoichiometry, and dielectric relaxation in B3.32M7.09O22.7 and structurally related ternary phases
【24h】

Crystal structure, stoichiometry, and dielectric relaxation in B3.32M7.09O22.7 and structurally related ternary phases

机译:B3.32M7.09O22.7和结构相关的三元相的晶体结构,化学计量和介电弛豫

获取原文
获取原文并翻译 | 示例
       

摘要

The crystal structure of the phase previously reported to occur at 4:9 Bi2O3:Nb2O5 has been determined using single-crystal X-ray and powder neutron diffraction (P6(3)/mmc; a = 7.4363(1)angstrom, c = 19.7587(5)angstrom; Z = 2). The structural study combined with phase equilibrium analyses indicate that the actual composition is B3.32Nb7.09O22.7. This binary compound is the end-member of a family of four phases which form along a line between it and the pyrochlore phase field in the Bi2O3:Fe2O3:Nb2O5 system. The structures are derived from the parent pyrochlore end-member by chemical twinning, and can also be described as unit-cell intergrowths of the pyrochlore and hexagonal tungsten bronze (HTB) structures. The dielectric properties of the three chemically twinned pyrochlore phases, B3.32Nb7.09O22.7, Bi9.3Fe1.1Nb16.9O57.8 and Bi5.67FeNb10O35, were characterized. All exhibit low-temperature, broad dielectric relaxation similar to that of the Bi-Fe-Nb-O pyrochlore. At 1 MHz and approximate to 175 K the observed relative permittivites were 345, 240, and 205, respectively, compared to 125 for the Bi-Fe-Nb-O pyrochlore. The higher relative permittivities observed for the chemically twinned pyrochlore derivatives are ascribed to the presence of HTB blocks in their structures: The Bi atoms located in the HT13 blocks feature highly asymmetric coordination environments compared to pyrochlore, and the magnitude of the relative permittivity increases with the proportion of Bi located within the HTB portions of the structures. (C) 2008 Elsevier Inc. All rights reserved.
机译:已使用单晶X射线和粉末中子衍射(P6(3)/ mmc; a = 7.4363(1)埃,c = 19.7587)确定了先前报道的以4:9 Bi2O3:Nb2O5出现的相的晶体结构(5)埃; Z = 2)。结构研究与相平衡分析相结合,表明实际组成为B3.32Nb7.09O22.7。该二元化合物是沿着Bi2O3:Fe2O3:Nb2O5系统中的四氯甲烷和烧绿石相场之间的直线形成的四族化合物的末端成员。这些结构是通过化学孪生从母体烧绿石末端成员衍生而来的,也可以描述为烧绿石和六边形钨青铜(HTB)结构的晶胞共生体。表征了三个化学孪生烧绿石相B3.32Nb7.09O22.7,Bi9.3Fe1.1Nb16.9O57.8和Bi5.67FeNb10O35的介电性能。它们都表现出类似于Bi-Fe-Nb-O烧绿石的低温宽介电弛豫。在1 MHz且接近175 K时,观察到的相对介电常数分别为345、240和205,而Bi-Fe-Nb-O烧绿石的相对介电常数为125。化学双联烧绿石衍生物观察到的较高相对介电常数归因于其结构中存在HTB嵌段:与烧绿石相比,位于HT13嵌段中的Bi原子具有高度不对称的配位环境,并且相对介电常数的大小随位于结构的HTB部分内的Bi的比例。 (C)2008 Elsevier Inc.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号