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New Lead Orthosilicate {Pb-4(?(?H)(2))}[SiO4] with a Framework of Anion-Centered Pb Tetrahedra Related to Sodalite

机译:新的铅外硅酸盐{Pb-4(?(αh)(2))} [SiO4]与与钠钠相关的阴离子为中心的Pb Tetrahedra框架

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New lead silicate {Pb-4(?(?H)(2))}[SiO4] was synthesized under hydrothermal conditions and structurally characterized, sp. gr. P2(1)3, a = 8.9756(13) angstrom. According to the commonly used classification, the new compound belongs to orthosilicates. In the crystal structure, isolated SiO4 tetrahedra are located between numerous Pb atoms. The structure can be considered as an anion-centered positively charged zeolite-like framework composed of {O3Pb7}(8+) clusters, which are linked to each other and include three edge-sharing (OPb4)(6+) tetrahedra with one common vertex. The formula of this positively charged antiframework is {O(?H)(2)Pb-4}(4+), and its cavities are occupied by negatively charged [SiO4](4-) tetrahedra. This framework is similar to that of sodalite when relating the sites to the centers of gravity of the {O3Pb7}(8+) clusters.
机译:在水热条件下合成新的铅硅酸盐{Pb-4(α(αH)(2))} [SiO 4]。 GR。 P2(1)3,A = 8.9756(13)埃。 根据常用的分类,新化合物属于矫形物。 在晶体结构中,分离的SiO 4四腹部位于众多PB原子之间。 该结构可以被认为是由{O 3P7}(8+)簇组成的基于带正电荷的沸石的框架,它们彼此连接,包括三个边缘共享(OPB4)(6+)四面体,其中一个常见 顶点。 该带正电荷的反r作业的公式是{O(αH)(2)Pb-4}(4+),其腔被带负电的[SiO 4](4-)四面体占据。 当将部位与{O3PB7}(8+)集群的重心相关联时,该框架类似于索索罗石。

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