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Crystal Structure of Alloriite

机译:变长石的晶体结构

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The cancrinite-sodalite group includes about 30 minerals, which are being studied in depth owing to their adsorption and ion-exchange properties. The minerals consist of a framework of Si and Al tetrahedra combined into six-membered rings. The rings of the same level along - are linked not to each other but to rings of neighbor levels shifted by 1/3 along x and y. The succession of alternation of rings is designated byrnletters A, B, and C, where A designates the rings around the axis [2/3 1/3 z]; B, around [1/3 2/3 z]; and C, around [0 0 z]. Minerals with 2 to 28 layers, which correspond to parameters with c ~5-74 A, are known in this group. The channels and cages within the framework are occupied by large cations and anions (mono- and/or multia-tom), while some minerals also include the water molecules.
机译:斜晶钠钙钠石组包含约30种矿物,由于其吸附和离子交换特性而正在深入研究。矿物质由Si和Al四面体的骨架组成,这些骨架结合成六元环。沿同一级别的环-彼此不链接,而是链接到沿x和y偏移1/3的相邻级别的环。环的交替顺序由字母A,B和C表示,其中A表示围绕轴[2/3 1/3 z]的环; B,大约[1/3 2/3 z];和C,在[0 0 z]左右。该组中已知有2至28层的矿物,对应于c〜5-74 A的参数。框架内的通道和笼子被大型阳离子和阴离子(单原子和/或多原子)占据,而某些矿物质还包括水分子。

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