Aqueous dissolution of Li-Na borosilicates: Insights from machine learning and experiments

•A normalised release feature was required for accurate B and Na ML predictions.•The absence of waste species yielded poor long-term 90 °C Li and Si ML predictions.•Faster kinetics for MW were due to glass and gel structure and precipitate changes.•BO3 leached preferentially and [BO4]− transformed n...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Journal of non-crystalline solids 2023-12, Vol.621, p.122630, Article 122630
Hauptverfasser: Goût, Thomas L., Lillington, Joseph N.P., Walden, James, Boukouvala, Christina, Ringe, Emilie, Harrison, Mike T., Farnan, Ian
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:•A normalised release feature was required for accurate B and Na ML predictions.•The absence of waste species yielded poor long-term 90 °C Li and Si ML predictions.•Faster kinetics for MW were due to glass and gel structure and precipitate changes.•BO3 leached preferentially and [BO4]− transformed near the surface during leaching.•Interdiffusion dominated dissolution, later changing to an ICDP model at 90 °C. Previously acquired data could be utilised in predicting glass dissolution kinetics at long times, but the application of machine learning methods needs to be assessed. Here, the dissolution processes of two Li-Na borosilicate ‘base glasses’ at 40 and 90 °C were investigated by SEM-EDS, NMR and Raman spectroscopy. Boron and sodium machine learning predictions were excellent when considering other normalised releases as features. However, extrapolating the training feature space yielded poorer performance and the absence of incorporated waste elements resulted in underestimated predicted long-term lithium and silicon releases. Faster dissolution kinetics were observed for MW than MW-½Li but the MW-½Li gel layer at 40 °C trapped more water. Whilst BO3 rings leached preferentially at 90 °C, surface enrichment of BO3 at 40 °C suggested [BO4]− transformed prior to dissolution. Results were consistent with interdiffusion being significant at 40 °C and interface-coupled dissolution precipitation beyond 7 days at 90 °C.
ISSN:0022-3093
1873-4812
DOI:10.1016/j.jnoncrysol.2023.122630