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首页> 外文期刊>Russian Journal of Inorganic Chemistry >Modeling of self-organization processes in crystal-forming systems: Symmetry and topology code for cluster self-assembly of crystal structures in MT-structures of polyvalent sulfates and phosphates
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Modeling of self-organization processes in crystal-forming systems: Symmetry and topology code for cluster self-assembly of crystal structures in MT-structures of polyvalent sulfates and phosphates

机译:晶体形成系统中自组织过程的模型:多价硫酸盐和磷酸盐的MT结构中晶体结构的簇自组装的对称性和拓扑代码

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摘要

We consider the supramolecular chemistry of polyvalent metal sulfates and phosphates built of M(n+)(O, OH, H2O)(6) polyhedral clusters with octahedral O-coordination (M-polyhedra) and SO4 and PO4 polyhedral clusters with tetrahedral O-coordination (T-polyhedra). These compounds form molecular (insular), chain, layered, or framework 3D MT structures by means of directed (bridging) hydrogen bonds O-HaEuro broken vertical bar O and/or bridging covalent O-bonds. Combinatorial-topological analysis algorithms are provided to restore, from structure data, the convergent matrix crystal structure self-assembly code. Cluster self-assembly modeling has been performed for the following sulfates: MgSO4 (Pnma and Cmcm), MgSO4 a (TM) 1H(2)O (Kieserite), and CuSO4 a (TM) 3H2O (Bonattite) having 3D MT strucutres; MgSO4 a (TM) 2H(2)O (Sanderite), MgSO4 center dot 2.5H(2)O, MnSO4 center dot 3H(2)O, and MnSO4(OH) center dot 2H(2)O having 2D MT structures; MgSO4 center dot 4H(2)O (Cranswickite) and MgSO4 center dot 5H(2)O (Pentahydrite) having 1D MT structures; and MgSO4 center dot 4H(2)O (Starkeyite) having a 0D MT structure, for the following phosphates: (VO)(HPO4) (P-1), MgSO4 center dot H2O (Kieserite), and CuSO4 center dot 3H(2)O (Bonattite) having 3D MT structures; (VO)(HPO4)(H2O)(0.5) (P121/c1 and Pmmn), (VO)(HPO4)(H2O)(2) (P4mm and P121/c1), V(3+)(PO4)(H2O)(2) (P1211), V(3+)(PO4)(H2O)(4) (C12/c1), and Mg(HPO4)(H2O)(3) (Newberyite, Pbca) having 2D MT structures; phosphite (VO(H2O)(2))(HPO3)(H2O)(3) (P4(1)) and phosphate (VO)(HPO4)(H2O)(4) (P-1) having 1D MT structures. For all compounds, the symmetry and combinatorial codes of cluster self-assembly code in the form of the following sequence: precursor nanocluster S (3) (0) -> primary chain S (3) (1) -> microlayer S (3) (2) -> microframework S (3) (3) . At the stage of primary chain S (3) (1) formation, in all of MT crystal structures considered, precursor clusters are four-polyhedral MTMT chains, transor cis, and their derivatives with additional O-bonds between polyhedra and ring cluster M2T2 (the result of coiling a cis-chain into a ring). Frequency analysis of topological and symmetry pathways in the formation and evolution of MT-clusters (from primary chain S (3) (1) through microlayer S (3) (2) to microframework S (3) (3) ) elucidates new crystal-formation trends in diverse chemical systems at the microscopic level.
机译:我们考虑了由具有八面体O配位(M-polyhedra)的M(n +)(O,OH,H2O)(6)多面体簇和具有四面体O配位的SO4和PO4多面体簇构成的多价金属硫酸盐和磷酸盐的超分子化学(T-多面体)。这些化合物通过定向(桥接)氢键O-HaEuro断开的垂直棒O和/或桥接共价O键形成分子(岛状),链状,层状或骨架3D MT结构。提供了组合拓扑分析算法,用于从结构数据中恢复会聚矩阵晶体结构的自组装代码。已经对以下硫酸盐进行了簇自组装建模:MgSO4(Pnma和Cmcm),MgSO4a(TM)1H(2)O(硅藻土)和CuSO4a(TM)3H2O(方钠石)具有3D MT结构。 MgSO 4 a(TM)2H(2)O(Sanderite),MgSO4中心点2.5H(2)O,MnSO4中心点3H(2)O和MnSO4(OH)中心点2H(2)O具有2D MT结构;具有一维MT结构的MgSO4中心点4H(2)O(Cranswickite)和MgSO4中心点5H(2)O(五水石);对于以下磷酸盐,具有0D MT结构的MgSO4中心点4H(2)O(Starkeyite):(VO)(HPO4)(P-1),MgSO4中心点H2O(Kieserite)和CuSO4中心点3H(2具有3D MT结构的)O(Bonattite); (VO)(HPO4)(H2O)(0.5)(P121 / c1和Pmmn),(VO)(HPO4)(H2O)(2)(P4 / nmm和P121 / c1),V(3 +)(PO4) (H2O)(2)(P121 / n1),V(3 +)(PO4)(H2O)(4)(C12 / c1)和Mg(HPO4)(H2O)(3)(Newberyite,Pbca)具有二维MT结构;亚磷酸盐(VO(H2O)(2))(HPO3)(H2O)(3)(P4(1))和具有一维MT结构的磷酸盐(VO)(HPO4)(H2O)(4)(P-1)。对于所有化合物,簇自组装代码的对称和组合代码按以下顺序形式:前体纳米簇S(3)(0)->主链S(3)(1)->微层S(3) (2)->微框架S(3)(3)。在形成主链S(3)(1)的阶段,在所有考虑的MT晶体结构中,前体簇是四面体MTMT链,反式顺式及其衍生物,在多面体和环簇M2T2之间具有附加的O键(将顺式链缠绕成环的结果)。 MT簇的形成和演化中的拓扑和对称路径的频率分析(从主链S(3)(1)到微层S(3)(2)到微框架S(3)(3))阐明了新的晶体-微观水平上各种化学系统中的形成趋势。

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