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Modelling regularity of Si/Al distributions in disordered tectosilicates - application to zeolites with the GIS
Montauban Moreira de Oliveira1, Jean Guillaume Eon1
1Instituto de Ciências Exatas, Matemática Pura, Universidade Federal Rural do Rio de Janeiro, P1-90-4, Seropédica, Rio de Janeiro 23890-000, Brazil.
Acta Crystallographica. Section A, Foundations and Advances
|August 15, 2025
Summary
This study introduces a new method to analyze silicon-aluminum ordering in tectosilicates. It reveals specific disordered substructures, termed alveoli, within these minerals, indicating partial order at the submicroscopic level.
Area of Science:
- Mineralogy
- Materials Science
- Crystallography
Background:
- Tectosilicates, including zeolites, exhibit complex silicon-aluminum ordering.
- Understanding this ordering is crucial for their properties and applications.
- Previous work established a foundation for analyzing these structures.
Purpose of the Study:
- To extend previous work by analyzing Si/Al distributions in tectosilicates.
- To develop and apply a novel method for characterizing order/disorder.
- To identify and describe submicroscopic ordered and disordered substructures.
Main Methods:
- Analysis of inter-relations between maximal independent sets.
- Utilizing a labelled quotient graph of the net.
- Application to various natural and synthetic tectosilicates, including GIS framework zeolites.
Main Results:
- Identification of specific disordered substructures, termed 'alveoli'.
- Demonstration of partial order in submicroscopic domains coexisting with ordered regions.
- Successful application to bikitaite, chabazite, analcime, gismondine, amicite, garronite, gobbinsite, and synthetic Na-P2.
Conclusions:
- The maximal independence principle applied to the labelled quotient graph effectively explains composition and order/disorder.
- The findings align well with existing 29Si magic-angle spinning NMR data.
- The method provides a robust framework for analyzing Si/Al distribution in tectosilicates.
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