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A structural model for charoite

机译:硅藻土的结构模型

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The crystal structure of charoite was investigated mainly by using selected-area electron diffraction (SAED), X-ray diffraction (XRD) and high-resolution electron microscopy (HREM). SAED and XRD patterns indicate that the structure has a monoclinic cell: a = 32.296, b = 19.651, c = 1.16 A, p = 96.3° and V= 4517 A~3. The space group inferred from systematic absences and HREM images is P2ilm. A model of the charoite structure is proposed that is based on the features of related Ca-alkaline silicate structures and HREM images. The structure of charoite consists of three different silicon-oxygen radicals (polymerized SiO_4 tetrahedra) which are located between Ca polyhedra. Two of these radicals form continuous tubular structures comprising pectolite-like tetrahedral chains. Calcium polyhedra are joined to form blocks, each of which consists of four columns sharing edges and apices. Potassium and H_2O molecules are probably located inside the tubular silicate radicals. From these results, a general formula is derived: K_(6-7)(Ca,Na)_(18)[(Si_6O_(17))(Si_(12)O_(30))(Si_(18)O_(45))](OH,F)_2-nH_2O with two formula units in the unit cell (Z = 2).
机译:主要通过选择区域电子衍射(SAED),X射线衍射(XRD)和高分辨率电子显微镜(HREM)研究了硫铝长石的晶体结构。 SAED和XRD图谱表明该结构具有单斜晶胞:a = 32.296,b = 19.651,c = 1.16A,p = 96.3°和V = 4517A〜3。从系统缺席和HREM图像推断出的空间群是P2ilm。基于相关的钙碱性硅酸盐结构和HREM图像的特征,提出了一种风碳石结构模型。硅藻土的结构由位于Ca多面体之间的三个不同的硅氧自由基(聚合的SiO_4四面体)组成。这些基团中的两个形成包含针孔状四面体链的连续管状结构。多面体钙被连接成块,每块由四列共享边和顶点的列组成。钾和H_2O分子可能位于管状硅酸盐自由基内部。从这些结果中得出一个通用公式:K_(6-7)(Ca,Na)_(18)[(Si_6O_(17))(Si_(12)O_(30))(Si_(18)O_(45 ))]](OH,F)_2-nH_2O,在单元格中具有两个公式单位(Z = 2)。

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