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Elastic behavior of MFI-type zeolites: 3 – Compressibility of silicalite and mutinaite

Authors :
Giovanna Vezzalini
Francesco Di Renzo
Simona Quartieri
Rossella Arletti
Vladimir Dmitriev
Dipartimento di Scienze della Terra
Universita degli Studi di Messina
Dipartimento di Scienze Mineralogiche e Petrologiche (DSMP)
Università degli studi di Torino (UNITO)
Dipartimento di Scienze della Terra [Modena]
Università degli Studi di Modena e Reggio Emilia (UNIMORE)
Institut Charles Gerhardt Montpellier - Institut de Chimie Moléculaire et des Matériaux de Montpellier (ICGM ICMMM)
Ecole Nationale Supérieure de Chimie de Montpellier (ENSCM)-Centre National de la Recherche Scientifique (CNRS)-Université de Montpellier (UM)-Université Montpellier 1 (UM1)-Université Montpellier 2 - Sciences et Techniques (UM2)-Institut de Chimie du CNRS (INC)
European Synchrotron Radiation Facility (ESRF)
Italian MIUR (PRIN2008)
Source :
Journal of Solid State Chemistry, Journal of Solid State Chemistry, Elsevier, 2012, 191, pp.201-212. ⟨10.1016/j.jssc.2012.03.039⟩
Publication Year :
2012
Publisher :
Elsevier BV, 2012.

Abstract

We report the results of an in-situ synchrotron X-ray powder diffraction study - performed using silicone oil as 'non-penetrating' pressure transmitting medium - of the elastic behavior of three zeolites with MFI-type framework: the natural zeolite mutinaite and two silicalites (labeled A and B) synthesized under different conditions. While in mutinaite no symmetry change is observed as a function of pressure, a phase transition from monoclinic (P2{sub 1}/n) to orthorhombic (Pnma) symmetry occurs at about 1.0 GPa in the silicalite samples. This phase transition is irreversible upon decompression. The second order bulk moduli of silicalite A and silicalite B, calculated after the fulfillment of the phase transition, are: K{sub 0}=18.2(2) and K{sub 0}=14.3 (2) GPa, respectively. These values makes silicalite the most compressible zeolite among those up to now studied in silicone oil. The structural deformations induced by HP in silicalite A were investigated by means of complete Rietveld structural refinements, before and after the phase transition, at P{sub amb} and 0.9 GPa, respectively. The elastic behaviors of the three MFI-type zeolites here investigated were compared with those of Na-ZSM-5 and H-ZSM-5, studied in similar experimental conditions: the two silicalites - which are the phases with the highest Si/Al ratiosmore » and hence the lowest extraframework contents - show the highest compressibility. On the contrary, the most rigid material is mutinaite, which has a very complex extraframework composition characterized by a high number of cations and water molecules. - Graphical abstract: High-pressure behavior of silicalite compressed in silicone oil: projection of the structure along the [0 1 0] direction at Pamb(a), 0.9 GPa (b). (c) Comparison of the unit-cell volume variations as a function of pressure for mutinaite, H-ZSM5, Na-ZSM5, silicalite A, and silicalite B compressed in silicone oil. Highlights: Black-Right-Pointing-Pointer X-ray powder diffraction study of silicalite and mutinaite compressibility. Black-Right-Pointing-Pointer Silicalite is the most compressible zeolite up to now studied. Black-Right-Pointing-Pointer A phase transition from monoclinic to orthorhombic symmetry occurs in silicalite. Black-Right-Pointing-Pointer Among MFI-type zeolites the most rigid material is mutinaite.« less

Details

ISSN :
00224596 and 1095726X
Volume :
191
Database :
OpenAIRE
Journal :
Journal of Solid State Chemistry
Accession number :
edsair.doi.dedup.....47aeb55d1063223c0b87a75b2ea53a5e