Crystal structures of K2[XSi5O12] (X = Fe2+, Co, Zn) and Rb2[XSi5O12] (X = Mn) leucites: comparison of monoclinic P21/c and Ia(3)over-bard polymorph structures and inverse relationship between tetrahedral cation (T = Si and X)-O bond distances and intertetrahedral T-O-T angles

被引:9
|
作者
Bell, Anthony M. T. [1 ]
Henderson, C. Michael B. [2 ,3 ]
机构
[1] Sheffield Hallam Univ, MERI, Sheffield S1 1WB, S Yorkshire, England
[2] Univ Manchester, Sch Earth & Environm Sci, Manchester M13 9PL, Lancs, England
[3] Sci & Technol Facil Council, Sci Tech Daresbury Lab, ASTeC, Warrington WA4 4AD, Cheshire, England
基金
英国工程与自然科学研究理事会;
关键词
X-ray powder diffraction; Rietveld; refinement; leucite-group minerals; silicate; framework structures; RAY-POWDER DIFFRACTION; RIETVELD REFINEMENT; ORTHORHOMBIC PBCA; ELASTIC BEHAVIOR; PHASE-TRANSITION; HIGH-PRESSURE; POLLUCITE; RB; NI; CS;
D O I
10.1107/S2052520618004092
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
The leucite tectosilicate mineral analogues K2X2+Si5O12 (X = Fe2+, Co, Zn) and Rb2X2+Si5O12 ( X = Mn) have been synthesized at elevated temperatures both dry at atmospheric pressure and at controlled water vapour pressure; for X = Co and Zn both dry and hydrothermally synthesized samples are available. Rietveld refinement of X-ray data for hydrothermal K2X2+Si5O12 (X = Fe2+, Co, Zn) samples shows that they crystallize in the monoclinic space group P2(1)/c and have tetrahedral cations ( Si and X) ordered onto distinct framework sites [cf. hydrothermal K2MgSi5O12; Bell et al. (1994a), Acta Cryst. B50, 560-566]. Drysynthesized K2X2+Si5O12 (X = Co, Zn) and Rb2X2+Si5O12 (X = Mn) samples crystallize in the cubic space group Ia (3) over bard and with Si and X cations disordered in the tetrahedral framework sites as typified by dry K2MgSi5O12. Both structure types have tetrahedrally coordinated SiO4 and XO4 sharing corners to form a partially substituted silicate framework. Extraframework K-vertical bar and Rb-vertical bar cations occupy large channels in the framework. Structural data for the ordered samples show that mean tetrahedral Si-O and X-O bond lengths cover the ranges 1.60 angstrom ( Si-O) to 2.24 angstrom (Fe2+-O) and show an inverse relationship with the intertetrahedral angles (T-O-T) which range from 144.7 degrees (Si-O-Si) to 124.6 degrees (Si-O-Fe2+).For the compositions with both disordered and ordered tetrahedral cation structures (K2MgSi5O12, K2CoSi5O12, K2ZnSi5O12, Rb2MnSi5O12 and Cs2CuSi5O12 leucites) the disordered polymorphs always have larger unit-cell volumes, larger intertetrahedral T-O-T angles and smaller mean T-O distances than their isochemical ordered polymorphs. The ordered samples clearly have more flexible frameworks than the disordered structures which allow the former to undergo a greater degree of tetrahedral collapse around the interframework cavity cations. Multivariant linear regression has been used to develop equations to predict intertetrahedral T-O-T angle variation depending on the independent variables Si-O and X-O bond lengths, cavity cation ideal radius, intratetrahedral (O-T-O) angle variance, and X cation electronegativity.
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页码:274 / 286
页数:13
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