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首页> 外文期刊>Doklady earth sciences >Crystal Structure of Yegorovite Na_4Si_4O_8(OH)_4 ? 7H_2O
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Crystal Structure of Yegorovite Na_4Si_4O_8(OH)_4 ? 7H_2O

机译:叶戈罗维石的晶体结构 Na_4Si_4O_8(OH)_4 ?7H_2O

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摘要

Using X-ray analysis, the crystal structure of yegorovite Na_4Si_4O_8(OH)_4 ? 7H_2O, a newly-discovered mineral from the Lovozero alkaline complex (Kola Peninsula, Russia), was determined. The mineral is monoclinic, of P2_1/c, a = 9.8744(4), b = 12.3981(5), c= 14.8973(7) A, β = 104.675(5)°, V=1764.29(13)A~3, Z = 4. Yegorovite is a representative of a new structure type. Its structure is based upon the zigzag chains Si_4O_8(OH)_4_∞ extended along 100. The Na atoms occupy four nonequivalent crystallographic positions and are located in six-fold polyhedra NaO(OH)_2(H_2O)_3 and NaO(OH)(H_2O)_4. The Na polyhedra are joined with each other by vertices and edges to form corrugated layers parallel to (001). To each of these layers, the silicon-oxygen chains adjoin from both sides, and the neighboring Na-Si layers are combined with one another by a system of H-bonds.
机译:利用X射线分析,yegorovite的晶体结构Na_4[Si_4O_8(OH)_4]?7H_2O,一种来自Lovozero碱性复合体(俄罗斯科拉半岛)的新发现的矿物被确定。矿物为单斜晶系,P2_1/c,a = 9.8744(4),b = 12.3981(5),c= 14.8973(7) A,β = 104.675(5)°,V=1764.29(13)A~3,Z = 4。Yegorovite是新结构类型的代表。它的结构基于沿[100]延伸的锯齿形链[Si_4O_8(OH)_4]_∞。Na 原子占据四个非等效晶体位置,位于六重多面体 [NaO(OH)_2(H_2O)_3] 和 [NaO(OH)(H_2O)_4] 中。Na 多面体通过顶点和边相互连接,形成平行于 (001) 的波纹层。对于这些层中的每一个,硅氧链从两侧相邻,相邻的Na-Si层通过氢键系统相互结合。

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