The incorporation of iron into peralkaline silicate glasses significantly impacts their structural and thermal properties. Here we investigate how addition of iron influences the network connectivity (short- and medium-range order) and glass transition temperature (Tg) with particular regard to the iron speciation and the Fe2+ and Fe3+ coordination state. We also found a sort of tipping point in iron concentration beyond which the short-range structures evolve linearly with density while the medium-range structure deviates from linearity. This behavior seems related to a re-enrichment of tetrahedral units triggered by iron self-compensation effect explaining the observed jump in Tg.
Fe-Dependent Structural Evolution of Peralkaline Soda Aluminosilicate Glasses: Iron Speciation vs. Glass Transition / Cassetta, M., De Bona, E., Sambugaro, A., Enrichi, F., Daldosso, N., Giannetta, B., Zaccone, C., Biesuz, M., Sglavo, V.M., Almeev, R., Nodari, L., Giordano, D., Mariotto, G.. - In: CHEMICAL GEOLOGY. - ISSN 0009-2541. - 2025, 674:(2025), pp. 1-10. [10.1016/j.chemgeo.2024.122561]
Fe-Dependent Structural Evolution of Peralkaline Soda Aluminosilicate Glasses: Iron Speciation vs. Glass Transition
Cassetta, Michele
Primo
;De Bona, EmanueleSecondo
;Daldosso, Nicola;Biesuz, Mattia;Sglavo, Vincenzo M.;Mariotto, Gino
2025-01-01
Abstract
The incorporation of iron into peralkaline silicate glasses significantly impacts their structural and thermal properties. Here we investigate how addition of iron influences the network connectivity (short- and medium-range order) and glass transition temperature (Tg) with particular regard to the iron speciation and the Fe2+ and Fe3+ coordination state. We also found a sort of tipping point in iron concentration beyond which the short-range structures evolve linearly with density while the medium-range structure deviates from linearity. This behavior seems related to a re-enrichment of tetrahedral units triggered by iron self-compensation effect explaining the observed jump in Tg.| File | Dimensione | Formato | |
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Descrizione: Chemical Geology Volume 674, 20 February 2025, 122561
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