Condensation of [Si<sub>3</sub>O<sub>9</sub>]<sup>6-</sup> Anions in the Solid State to the Dimeric Cyclotrisilicate Anion [Si<sub>6</sub>O<sub>17</sub>]<sup>10-</sup>
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The structure of the silicate Rb10[Si6O17] containing a novel dimeric cyclotrisilicate anion is reported. The compound is formed by the reaction of a mixture of SiO2 and Rb at temperatures above 700 °C. Systematic investigations by means of differential thermal analysis and temperature-dependent powder X-ray diffraction experiments revealed that the new compound evolved from Rb6[Si3O9], which occurred as an intermediate product. Thus, the dimeric anion [Si6O17]10- is formed by condensation of the monomeric cyclotrisilicate [Si3O9]6-. For both silicates, [Si6O17]10- and [Si3O9]6-, the characteristic ring vibration modes were observed in the IR spectrum. The structure of Rb10[Si6O17] was solved and refined from single-crystal X-ray diffraction data in the orthorhombic space group Pbca (No. 61). Synthesis and structure determination of Rb10[Si6O17] bridge the gap to show that the recently reported structures of Rb14[Si4][Si6O17] and Rb14[Ge4][Si6O17] are indeed fascinating intergrowth structures of the stable oxide Rb10[Si6O17] and the Zintl phases RbSi (Rb4Si4) and RbGe (Rb4Ge4), respectively.



