Fe-dependent structural evolution of peralkaline soda aluminosilicate glasses: Iron speciation vs. glass transition

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 ( T g ) with particular regard to the iron speciation and the Fe 2+ and Fe 3+ 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. This behavior seems related to a re-enrichment of tetrahedral units triggered by iron self-compensation effect explaining the observed jump in T g .

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Publication Details

Journal
Chemical Geology
Published
2024-12-11
DOI
https://doi.org/10.1016/j.chemgeo.2024.122561
Citations
7
Primary Topic
Glass properties and applications
Type
article
Field-Weighted Citation Impact
1.64

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article

Fe-dependent structural evolution of peralkaline soda aluminosilicate glasses: Iron speciation vs. glass transition

Vincenzo M. Sglavo, Renat Almeev, Beatrice Giannetta, N. Daldosso et al.
7 citations
Chemical Geology
Glass properties and applications
1.64
article

Fe-dependent structural evolution of peralkaline soda aluminosilicate glasses: Iron speciation vs. glass transition

Vincenzo M. Sglavo, Renat Almeev, Beatrice Giannetta, N. Daldosso, Michele Cassetta, Francesco Enrichi, Luca Nodari, Claudio Zaccone, G. Mariotto, Mattia Biesuz, Emanuele De Bona, Daniele Giordano, Alessia Sambugaro
article en
7 citations

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 ( T g ) with particular regard to the iron speciation and the Fe 2+ and Fe 3+ 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. This behavior seems related to a re-enrichment of tetrahedral units triggered by iron self-compensation effect explaining the observed jump in T g .

Chemical GeologyVol. 674
University of Foggia (IT), Leibniz University Hannover (DE), University of Verona (IT), University of Trento (IT), Istituto Nazionale di Geofisica e Vulcanologia (IT), Institute of Geosciences and Earth Resources (IT), Institute of Science and Technology for Ceramics (IT), Institute of Condensed Matter Chemistry and Technologies for Energy (IT), Torino e-district (IT), National Research Council (IT), University of Turin (IT)
European Commission, Deutsche Forschungsgemeinschaft
Openalex Percentile: Top 20%
Glass properties and applications
1.64
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