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Chin. Phys. B, 2026, Vol. 35(5): 056102    DOI: 10.1088/1674-1056/ae3606
SPECIAL TOPIC — John Tse: Pioneer in high-pressure materials science Prev   Next  

Free oxide ion abundances in Na, Ba, and K silicate glasses from O 1s XPS, 29Si NMR, Raman, and MD simulations

G. Michael Bancroft1,†, H. Wayne Nesbitt2, John S. Tse3, Grant S. Henderson4, and Ben J. A. Moulton5
1 Department of Chemistry, University of Western Ontario, London, ON N6A 5B7 Canada;
2 Department of Earth Sciences, University of Western Ontario, London, ON N6A 5B7 Canada;
3 Department of Physics and Engineering Physics, University of Saskatchewan, Saskatoon, SASK S7N 5E2 Canada;
4 Department of Earth Sciences, University of Toronto, Toronto, ON M5S 3B1 Canada;
5 Inamori School of Engineering, New York College of Ceramics, Alfred University, Alfred, New York 14802 USA
Abstract  In alkali silicate glasses with $\le 50$ mol% $M_{2}$O ($M={\rm Na}$, K, Rb, Cs), the existence of $>1$ mol% reactive ``free'' oxide (FO, where O is not bonded to Si) has been a highly controversial topic over the past 15 years. Unlike their crystalline analogues, Raman and $^{29}$Si nuclear magnetic resonance (NMR) studies since 1980 have shown that two or more $Q^{n}$ ($n=$0-4) species are present in silicate glasses over a wide range of compositions. For example, $M_{2}$SiO$_{3}$ crystals contain only $Q^{2}$ species; however, glasses of the same composition exhibit $Q^{1}$ and $Q^{3}$ in addition to $Q^{2}$. Previous Raman and NMR studies on alkali silicate glasses have related the abundances of these three species solely through disproportionation reactions (e.g. $2{ Q}^{2}\Leftrightarrow { Q}^{1}+{ Q}^{3}$). In doing so, polymerization reactions (e.g. $2{ Q}^{2}\Leftrightarrow 2{ Q}^{3}+{\rm FO}$) were completely neglected. By combining published O 1s x-ray photoelectron spectroscopy (XPS) spectra, $^{29}$Si NMR and Raman results for 40 mol% and 50 mol% Na$_{2}$O, K$_{2}$O, and BaO glasses, together with new molecular dynamics (MD) simulations of Na$_{4}$SiO$_{4}$ glass, we provide consistent and compelling evidence for the existence of $>1$ mol% FO in these glasses and melts. In particular, for 50 mol% K$_{2}$O silicate glass, all three experimental techniques estimate FO to be $\ge 7$ mol%, while MD simulations of Na$_{4}$SiO$_{4}$ yield $\sim 5$ mol% FO. Our analysis requires revised assignments (challenging decades of ``conventional wisdom'') for $^{29}$Si NMR and Raman spectra, based on O mass balance, recognition of M-BO bonding effects first identified in O 1s XPS spectra, and quantitative analysis of Raman spectra for 40-50 mol% Na$_{2}$O, K$_{2}$O, and BaO glasses. These FO values are comparable to those now accepted for alkaline-earth silicate glasses. The importance of this reactive FO for chemical reactivity (e.g. with H$_{2}$O and CO$_{2}$), bioactivity, and physical properties (e.g. melting) of silicate glasses is discussed.
Keywords:  alkali silicate glasses      free oxide (Na-O-Na)      O 1s XPS      Raman      $^{{29}}$Si NMR  
Received:  23 October 2025      Revised:  06 January 2026      Accepted manuscript online:  09 January 2026
PACS:  61.43. Fs  
  79.60.-i (Photoemission and photoelectron spectra)  
  76.60.-k (Nuclear magnetic resonance and relaxation)  
  78.30.-j (Infrared and Raman spectra)  
Corresponding Authors:  G. Michael Bancroft     E-mail:  gmbancro@uwo.ca

Cite this article: 

G. Michael Bancroft, H. Wayne Nesbitt, John S. Tse, Grant S. Henderson, and Ben J. A. Moulton Free oxide ion abundances in Na, Ba, and K silicate glasses from O 1s XPS, 29Si NMR, Raman, and MD simulations 2026 Chin. Phys. B 35 056102

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