1991
DOI: 10.1016/s0277-5387(00)83547-0
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The chemistry of simple ceramic glazes—III. A MASNMR study of simulated feldspars and their reactions with CaO, SrO, BaO or Li2O on heating to 1300°C

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Cited by 3 publications
(3 citation statements)
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“…Forcing water into an albite melt at high pressure and then quenching surprisingly caused no network depolymerization although the 27A1 NMR linewidth did decrease with increasing water content indicafing a reduction in Cq [203]. Addition of CaO, Li20, BaO and SrO to synthetic albite glasses induced ordering of the glass, and, at > 80 mol% CaO caused crystaUization and phase separation [204].…”
Section: Aluminosilicate Glasses Gels and Fibresmentioning
confidence: 96%
“…Forcing water into an albite melt at high pressure and then quenching surprisingly caused no network depolymerization although the 27A1 NMR linewidth did decrease with increasing water content indicafing a reduction in Cq [203]. Addition of CaO, Li20, BaO and SrO to synthetic albite glasses induced ordering of the glass, and, at > 80 mol% CaO caused crystaUization and phase separation [204].…”
Section: Aluminosilicate Glasses Gels and Fibresmentioning
confidence: 96%
“…The chemical shift of 104 ppm correspond to Q 4 (1Al). The peaks at around 89 to 90 ppm, could be assigned to Q 4 (3Al) indicating further ordering of the aluminosilicate network [23]. The peak of 70 ppm for G1 glaze can be assigned to Q 1 .…”
mentioning
confidence: 96%
“…The spectrum for glaze G1 has three Gaussian peaks, while two Gaussian peaks are necessary to simulate the spectra from glazes G2 and G3 as can be seen in figure 7. Standard glaze G0 gives a chemical shift of 96 ppm which could be assigned to Q 4 (2Al) site [23]. Alkali and alkaline earth aluminosilicate glasses generally show peaks that can be assigned to Q 4 (2Al) and Q 4 (3Al) sites [24].…”
mentioning
confidence: 99%