2012
DOI: 10.1016/j.jssc.2012.03.039
|View full text |Cite
|
Sign up to set email alerts
|

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

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
4
1

Citation Types

8
40
1

Year Published

2013
2013
2020
2020

Publication Types

Select...
6
1

Relationship

1
6

Authors

Journals

citations
Cited by 21 publications
(49 citation statements)
references
References 30 publications
(44 reference statements)
8
40
1
Order By: Relevance
“…In fact, in the same P range, the volume variation is about 5% for silicalite-1 F and silicalite-1 OH, 9 2.6% for siliceous Y, 69 and 3.96% for Si-ferrierite. 68 Since MOR has a 'framework density' (FD 47 ) much higher than zeolite Y (17.2 and 12.7, respectively), these results confirm once again that zeolite compressibility is not simply related to the material porosity.…”
Section: Discussionmentioning
confidence: 89%
See 2 more Smart Citations
“…In fact, in the same P range, the volume variation is about 5% for silicalite-1 F and silicalite-1 OH, 9 2.6% for siliceous Y, 69 and 3.96% for Si-ferrierite. 68 Since MOR has a 'framework density' (FD 47 ) much higher than zeolite Y (17.2 and 12.7, respectively), these results confirm once again that zeolite compressibility is not simply related to the material porosity.…”
Section: Discussionmentioning
confidence: 89%
“…As a consequence, some zeolites characterized by large pores can be unexpectedly less compressible than other pure-Si phases with empty cavities. Various authors [7][8][9][10][11][12][13] came to the same conclusions working on materials sharing the same framework type, but with different extra-frameworks and framework compositions. The compression of zeolites using non-penetrating media has also been exploited to induce the so-called ''pressureinduced amorphization'' (PIA).…”
Section: Introductionmentioning
confidence: 90%
See 1 more Smart Citation
“…The former are usually aqueous/alcohol mixtures, with molecular sizes small enough to penetrate the zeolite porosities (see for example [15] and [16] for a review); the latter are usually silicone oil or glycerol, with molecules too large to penetrate the zeolite (see e.g. [14,[17][18][19][20][21][22][23][24]). While non-penetrating PTM are mainly used to study zeolite compressibility, Pinduced phase transitions, and amorphization, the penetrating ones can be usefully exploited for investigating the so-called pressure induced hydration (PIH) effect [25], which consists in the penetration of additional H 2 O molecules into the zeolite channels.…”
Section: Introductionmentioning
confidence: 99%
“…The interest in the confinement of water in nanoscopic spaces, like zeolitic cavities, stems from the fact that the properties of confined water are believed to be very different from those of the bulk fluid. Finally, it has been shown that the intrusion of extra-guest species into zeolite cavities also has important consequences on the overall elastic behavior of the material, since the new guest molecules generally contribute to stiffening the structure and countering P-induced deformations [18,23,24,[27][28][29].…”
Section: Introductionmentioning
confidence: 99%