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Insight on MWW siliceous zeolites: from 2D precursors toward 3D structure
Francesca Rosso, Alessia Airi, Matteo Signorile, Eddy Dib, Silvia Bordiga, Valentina Crocellà, Svetlana Mintova, Francesca Bonino

Insight on MWW siliceous zeolites: from 2D precursors toward 3D structure

Science & Mathematics Published 2024 Verification Pending

Overview & Synopsis

ITQ-1 layered zeolites, with MWW framework, were prepared using different synthesis and calcination procedures and fully characterized by means of X-ray diffraction, scanning electron microscopy, N2 sorption and vibrational and nuclear magnetic resonance spectroscopies. Exploring different compositions of the precursor gel, the role of the Organic Structure Directing Agent (OSDA) was definitely disclosed. We proved that the concentration of OSDA in the synthesis gel affects the short-range crystalline order of zeolite crystals. In particular, diluted precursor gels led to the formation of low-density materials in the form of hollow spheres, with partially disordered layers, thinner crystals and high defectivity. In general, all ITQ-1 samples had the same crystalline structure but different morphology, either rose-like or hollow spheres. Moreover, the calcination procedure had an impact on the structural defects of the ITQ-1 zeolite: the higher the removal rate of the OSDA, the higher the defectivity degree of the zeolite.

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Document Information

Document Title Insight on MWW siliceous zeolites: from 2D precursors toward 3D structure
Author / Organization Francesca Rosso, Alessia Airi, Matteo Signorile, Eddy Dib, Silvia Bordiga, Valentina Crocellà, Svetlana Mintova, Francesca Bonino
Subject & Discipline Multidisciplinary Academic Open Research
Categories Science & Mathematics
Publication Year 2024
License / Rights Open Access / Creative Commons
Resource Verification Listed PDF (Verification Pending)
Original Host Website HAL Open Science (hal.science)
File Format application/pdf (Portable Document Format)
Language EN
Catalog ID DOC-33084
Original Source Link Visit Source Page on hal.science »