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Gatta, G. D., Lee, Y. (2014) Zeolites at high pressure: A review. Mineralogical Magazine, 78 (2) 267-291 doi:10.1180/minmag.2014.078.2.04

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Reference TypeJournal (article/letter/editorial)
TitleZeolites at high pressure: A review
JournalMineralogical Magazine
AuthorsGatta, G. D.Author
Lee, Y.Author
Year2014 (April)Volume78
Issue2
PublisherMineralogical Society
DOIdoi:10.1180/minmag.2014.078.2.04Search in ResearchGate
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Mindat Ref. ID244501Long-form Identifiermindat:1:5:244501:8
GUID0
Full ReferenceGatta, G. D., Lee, Y. (2014) Zeolites at high pressure: A review. Mineralogical Magazine, 78 (2) 267-291 doi:10.1180/minmag.2014.078.2.04
Plain TextGatta, G. D., Lee, Y. (2014) Zeolites at high pressure: A review. Mineralogical Magazine, 78 (2) 267-291 doi:10.1180/minmag.2014.078.2.04
Abstract/NotesAbstractThis is a review of the elastic behaviour and pressure (P)-induced structural evolution of zeolites and presents a comparative analysis of the deformation mechanisms of the Si/Al-framework and the rearrangement of the extra-framework species in response to applied pressure. The interaction betweenP-transmitting fluids and zeolites, which can lead to phenomena such as ‘P-induced over-hydration’, is described. The comparative elastic analysis and the high-Pstructural data of zeolites reported so far allow us to make some generalizations: (1) The range of compressibility among this class of openframework silicates is large, with bulk moduli ranging between 15 and 70 GPa; (2) Microporosity does not necessarily imply high compressibility, as several zeolites are less compressible than other nonzeolitic rock-forming minerals; (3) Compressibilities of zeolites do not seem to be directly related to microporosity, at least if we model microporosity with the ‘framework density’; (4) The flexibility observed in zeolites under hydrostatic compression is mainly governed by tilting of rigid tetrahedra around O atoms that behave as hinges within the framework. Pressure-induced tilting commonly leads to continuous rearrangement of the framework without any phase transition. More rarely, tilting induces displacive phase transitions and isothermalP-induced reconstructive phase transitions (i.e. with change in framework topology), have not been reported in this class of materials; (5) Deformation mechanisms in response to applied pressure are generally dictated by the topological configuration of the framework rather than the Si/Al-distribution or the extra-framework content. The channel content governs the compressibility of the cavities, leading to different unit-cell-volume compressibilities in isotypic structures.


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