2010
DOI: 10.1016/j.micromeso.2010.07.023
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Pressure-induced hydration and cation migration in a Cs+ exchanged gallosilicate zeolite LTL: Synchrotron X-ray powder diffraction study at ambient and high pressures

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Cited by 12 publications
(7 citation statements)
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“…Several zeolites were amorphized under high pressure, i.e., pressure-induced full or partial amorphization reverting back to the original crystalline structure upon decompression [15,16]. The partly disordered structure resulted from the local collapse and distortion of zeolite framework, which 4 was closely related to the properties of charge-balancing cations in the zeolites [17]. Lee et al reported that high pressure of 1.9 GPa led to the irreversible migration and rearrangement of charge-balancing cations, i.e., pressure-induced migration, and to the formation of super-hydrated zeolite with a doubled water content described as pressure-induced hydration [18].…”
Section: Introductionmentioning
confidence: 99%
“…Several zeolites were amorphized under high pressure, i.e., pressure-induced full or partial amorphization reverting back to the original crystalline structure upon decompression [15,16]. The partly disordered structure resulted from the local collapse and distortion of zeolite framework, which 4 was closely related to the properties of charge-balancing cations in the zeolites [17]. Lee et al reported that high pressure of 1.9 GPa led to the irreversible migration and rearrangement of charge-balancing cations, i.e., pressure-induced migration, and to the formation of super-hydrated zeolite with a doubled water content described as pressure-induced hydration [18].…”
Section: Introductionmentioning
confidence: 99%
“…Experimentally, framework flexibility can be probed by applying external pressure and studying the response of the structure. The mechanical behaviour of zeolites can be strongly influenced by the extra-framework content, such as occluded structure-directing cations [7,22,23,24] and organic additives [25], and connections between framework flexibility and guest structure-directing species can in principle provide valuable insights into the nature of the TO 4 clathration process during crystallisation.…”
Section: Introductionmentioning
confidence: 99%
“…[24] Our refinement models show that site C is susceptible to exchange with Cs + ions and is similarly populated to its gallosilicate analogue, reported by Seoung et al, to have a 50:50 fractional occupancy at this same site. [25] It is also important to note that the overall occupancy at site C by K + and Cs + ions combined is 0.83 per unit-cell compared to the full occupancy by K + ions in the parent K-L zeolite. To render an overall neutral structure, this is compensated for by the increased overall occupancy at site D which is 0.72 Cs + per unit-cell compared to the 0.63 K + in the parent K-L zeolite.…”
Section: Resultsmentioning
confidence: 99%