The new oxosilicate NaTbSi2O6: A comparison of its A- and D-type structure
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Marion C. Schäfer
Abstract
Two different modifications of the composition NaTbSi2O6 were synthesized within the class of quaternary alkali-metal rare-earth metal(III) oxosilicates. Monoclinic NaTbSi2O6 (A-type structure: space group P21/c (no. 14); a = 542.57(4), b = 1376.54(9), c = 762.83(5) pm, β = 110.086(3)°, Vm = 80.557(9) cm3/mol, Z = 4) crystallizes isotypically with NaYSi2O6 und LiScSi2O6. In this ino-oxosilicate, the [SiO4]4– tetrahedra are vertex-shared and linked to form infinite zigzag chains ∞1{[SiO2/2vO2/1t]2–} along [001]. Both, the Na+ and the Tb3+ cations are coordinated by seven O2– anions each. The [TbO7]11– polyhedra get connected via trans-oriented edges to build up ∞1{[TbO4/2eO3/1t]7–} chains running along [001], which alternate with the ∞1{[SiO2/2vO2/1t]2–} chains. In contrast, triclinic NaTbSi2O6 with a novel D-type structure (space group: P-1 (no. 2), a = 549.41(4), b = 938.65(6), c = 972.30(7) pm, α = 117.263(2), β = 97.239(2), γ = 99.676(2)°, Vm = 85.798(9) cm3/mol, Z = 3) belongs to the cyclo-oxosilicates according to Na3Tb3[Si6O18] with Z = 1. The arrangement of the resulting corrugated six-membered [Si6O18]12– rings of vertex-shared [SiO4]4– tetrahedra is similar to a hexagonal closest packing parallel to (100). The two types of distorted [TbO6]9– octahedra are linked along [010] via common edges to form undulated infinite ∞1{[TbO4/2vO2/1t]5–} chains, which become alternatingly piled with the cyclo-[Si6O18]12– units and the incorporated Na+ cations along [010]. While the square-pyramidally coordinated (Na2)+ cations are situated between the isolated cyclo-oxohexasilicate anions, the sixfold coordinated (Na1)+ cations can be found inside the rings. They are therefore surrounded by the six bridging O2– anions of the cyclo-[Si6O18]12– units in a quasi-planar hexagonal coordination sphere.
© by Oldenbourg Wissenschaftsverlag, München, Germany
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