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首页> 外文期刊>International Journal of Quantum Chemistry >SYNTHESIS AND STRUCTURAL CHARACTERIZATION OF La4Mn3Ge5.2Si0.8O22, A NEW COMPOUND WITH THE PERRIERITE STRUCTURE
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SYNTHESIS AND STRUCTURAL CHARACTERIZATION OF La4Mn3Ge5.2Si0.8O22, A NEW COMPOUND WITH THE PERRIERITE STRUCTURE

机译:珍珠岩结构的新型化合物La4Mn3Ge5.2Si0.8O22的合成与结构表征

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摘要

A new layered germanate La4Mn3Ge5.2Si0.8O22 has been prepared and its structure was determined from single crystal diffraction data. This compound crystallizes in the monoclinic space group P21/c with a=11.956(2) angstroms, b=5.642(1) angstroms, c=14.180(3) angstroms, beta=114 degrees09(3), and Z=2 formula units by cell. The structure has been refined to residuals of R=3.14% for 1380 observations and 152 parameters. La4Mn3Ge5.2Si0.8O22 is isostructural with perrierite Ce4Fe2 Ti3Si4O22, a naturally occurring sorosilicate mineral. The framework consists of rutile-like slabs formed of alternating chains of GeO6 octahedra and Mn3+O6 distorted octahedra, located between layers of mixed Ge1.2Si0.8O7 disilicates groups that separate the isolated Mn2+O6 octahedra. A structural comparison with La4Mn5Si4O22 is discussed. 21 refs.
机译:制备了新的层状锗酸盐La4Mn3Ge5.2Si0.8O22,并根据单晶衍射数据确定了其结构。该化合物在单斜空间群P21 / c中以a = 11.956(2)埃,b = 5.642(1)埃,c = 14.180(3)埃,β= 114度09(3)和Z = 2公式单位结晶按单元。对于1380个观测值和152个参数,该结构已精炼为R = 3.14%的残差。 La4Mn3Ge5.2Si0.8O22与钙钛矿Ce4Fe2 Ti3Si4O22(一种天然存在的硅酸盐矿物)同构。该框架由类似金红石的平板组成,由交替排列的GeO6八面体和Mn3 + O6扭曲的八面体的交替链形成,位于混合的Ge1.2Si0.8O7二硅酸盐基团的层之间,分隔分离的Mn2 + O6八面体。讨论了与La4Mn5Si4O22的结构比较。 21个参考

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