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Silicon-29 NMR studies of aqueous silicate solutions. 1. Chemical shifts and equilibria

Journal Article · · Inorg. Chem.; (United States)
DOI:https://doi.org/10.1021/ic00296a034· OSTI ID:5974314
In the /sup 29/Si NMR spectra of aqueous alkali-metal (M) silicate solutions ((MOH):(Si/sup IV/) = 1.0 or higher), variations in solution composition cause displacements of the peaks of up to 1 ppm largely through interaction of silicate units with M/sup +/. The analysis of the chemical shift data provides a means of predicting /sup 29/Si resonance frequencies for new silicate species and has aided in the identification of the Si/sub 4/O/sub 10//sup 4/minus// (Q/sub 4//sup 3/) anion, in which the Si atoms are at the corners of a regular tetrahedron. A quantitative study of the dependence of silicate connectivity upon temperature (-5 to +144 /degree/C) and solution composition shows that silicate polymerization is favored by low temperature, low alkalinity, and high (Si/sup IV/). In no case could silicate centers with 4-fold connectivity (Q/sup 4/) be detected. The effect of M/sup +/ on the distributions of silica species is small, but the larger M/sup +/ atoms do preferentially stabilize the more highly polymerized silicate anions. 35 refs., 8 figs., 3 tabs.
Research Organization:
Univ. of Calgary, Alberta (Canada)
OSTI ID:
5974314
Journal Information:
Inorg. Chem.; (United States), Journal Name: Inorg. Chem.; (United States) Vol. 27:23; ISSN INOCA
Country of Publication:
United States
Language:
English