Synthesis, crystal structure, and vibrational spectroscopy of K(2)Ca(4)Si(8)O(21)--an unusual single-layer silicate containing Q(2) and Q(3) units.
Single crystals of the previously unknown potassium calcium silicate K2Ca4Si8O21 (1) have been grown from a nonstochiometric melt as well as using a KCl flux. The compound is triclinic with the following basic crystallographic data: space group P, a = 6.8052(3) A, b = 7.1049(3) A, c = 11.2132(5) A, alpha = 96.680(4)degrees, beta = 105.280(4) degrees, gamma = 109.259(4)degrees, Z = 1, V = 481.28(4) A3. The crystal structure was solved by direct methods based on a single-crystal diffraction data set collected at ambient conditions. From a structural point of view, K2Ca4Si8O21 belongs to the group of single-layer silicates. The layers parallel to (001) are characterized by a complex arrangement of 6-, 8-, 10-, and 12-membered tetrahedral rings. The sheets can be built from the condensation of loop-branched fnfer single chains running parallel to [100], i.e., the crystallochemical formula can be written as K2Ca4{lB,5, 1(infinity)2}[Si8O21]. Compound 1 is the first example of a loop-branched layer silicate containing secondary (Q2) as well as tertiary (Q3) tetrahedra. Linkage between the layers is provided by calcium and potassium cations, which are distributed among a total of three crystallographically independent nontetrahedral sites. Alternatively, the structure can be described as a heteropolyhedral framework, based on SiO4 tetrahedra and CaO6 octahedra. The irregularly coordinated K-cations in turn are incorporated in tunnels of the network running parallel to [110]. The structural investigations have been completed by Raman spectroscopy. The allocation of the bands to certain vibrational species has been aided by density functional theory (DFT) calculations.
Arroyabe
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Institute of Mineralogy and Petrography, University of Innsbruck, Innrain 52, A-6020 Innsbruck, Austria.
Kaindl
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Többens
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Kahlenberg
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