Abstract
The compounds crystallizing in the system KOH–TiO2(rutile)–GeO2(quartz structure)–H2O at 500°C, 0.1 GPa, and different TiO2 : GeO2 ratios (1 : 1 to 1 : 6) and KOH concentrations (5–40 wt %) are R-GeO2 (rutile structure), K2Ti6O13 (analog of the mineral jeppeite), K2Ge[6]Ge3 [4]O9, and K3HGe4 [6]Ge3 [4]O16 · 4H2O (superscripts specify the oxygen coordination of Ge). The dominant phase is K2Ti6O13, which has a three-dimensional framework structure made up of corner- and edge-shared TiO6 (M) octahedra. The matrix-assembly model is used to examine the formation of the K2Ti6O13 structure from K4 M 12 = 2K2 M 6 subpolyhedral structural units resulting from the condensation of two flat 2M × 3M (six octahedra) blocks.
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Ilyushin, G.D. Hydrothermal Crystallization in the System KOH–TiO2–GeO2–H2O at 500°C and 0.1 GPa. Inorganic Materials 39, 951–958 (2003). https://doi.org/10.1023/A:1025561322644
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DOI: https://doi.org/10.1023/A:1025561322644