Pentacoordinate acyclic and cyclic anionic oxysilicates. A 29 si nmr and x-ray structural study1, 2

Abstract

Variable temperature -29 Si NMR spectral measurements revealed the formation of acyclic anionic silicates, [R,', Si(OR)5- n][K, 18-crown-6], n - 0-3, from reactions of alkoxy and aryloxysilanes with the respective potassium alkoxide or potassium aryloxide in the presence of 18-crown-6. This elusive class of substances has been proposed as model intermediates in the sol-gel process. In the case of (PhSi(OCH2CF3)4][K, 18-crown-6], isolation as a crystalline solid was achieved. The 29 Si chemical shifts move progressively downfield from Si(OR)5- to R'Si(OR)4- to R'2Si(OR)3-. Pentaalkoxysilicate anions react rapidly with pinacol to form the corresponding five-coordinated bicyclic anionic silicate. Independent synthesis and an X-ray structural study verified the formation of the bis(pinacolate),[(Me4C2O2)2SiO-i-Pr][K, 18-C-6] (1). For comparison of structural distortions, the synthetic and X-ray characterization of the related anionic oxysilicates, [(C6H4(CF3)2CO)2SiC6H11][Et4N] (2) and [(CH4O2)2SiC6H11][Me2NH2] (3), are reported. The structures of 1 and 2 are trigonal-bipyramidal and that of 3 is rectangular-pyramidal. The silicate 1 crystallizes in the monoclinic space group P21/n witha = 10. 314 (3) Å, b = 20. 401 (5)Å, c = 16.608 (4) Å, β = 91.04 (2)°, and Z = 4. Silicate 2 crystallizes in the monoclinic space group P21 with a = 10. 148 (2) Å, b = 16. 356 (6) Å, c = 11. 266 (3) Å, β =114.02 (2)°, and Z = 2. The bis catecholate 3 crystallizes in the monoclinic space group P21/c with a = 13. 566 (2) Å, b = 14. 962 (3) Å, c = 20. 561 (4) Å, β = 103.56 (1)°, and Z = 8. The final conventional unweighted residuals are 0.047 (1), 0.060 (2), and 0.059 (3). © 1995, Taylor & Francis Group, LLC. All rights reserved.