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首页> 外文期刊>Doklady Earth Sciences >Crystal Structure of Yegorovite Na_4[Si_4O_8(OH)_4] • 7H_2O
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Crystal Structure of Yegorovite Na_4[Si_4O_8(OH)_4] • 7H_2O

机译:钠铁矾Na_4 [Si_4O_8(OH)_4]•7H_2O的晶体结构

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摘要

Using X-ray analysis, the crystal structure of yegorovite Na_4[Si_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:使用X射线分析,确定了从Lovozero碱性复合物(俄罗斯科拉半岛)中新发现的矿物–钙铁辉石Na_4 [Si_4O_8(OH)_4]•7H_2O的晶体结构。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。叶绿铁矿是新结构类型的代表。它的结构基于沿着[100]延伸的锯齿形[Si_4O_8(OH)_4]_∞。 Na原子占据四个非等价晶体位置,并位于六倍多面体[NaO(OH)_2(H_2O)_3]和[NaO(OH)(H_2O)_4]中。 Na多面体通过顶点和边缘彼此结合以形成平行于(001)的波纹层。对于这些层中的每一层,硅-氧链从两侧邻接,并且相邻的Na-Si层通过H键系统相互结合。

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