2004
DOI: 10.1002/cphc.200400195
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A Numerical Evidence for Nonframework Cation Redistribution Upon Water Adsorption in Faujasite Zeolite

Abstract: Trace amounts of water are sufficient to produce cation redistribution in zeolites. Monte Carlo simulations of zeolite faujasite NaY reveal a spontaneous redistribution of site‐I and site‐I′ cations upon water adsorption. When aromatics are coadsorbed in the zeolite, cation redistribution takes place for a very small amount of water (full dots in the figure).

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Cited by 41 publications
(60 citation statements)
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“…in so called sites I'). [31] It is worth noticing that the water fills the porous volume homogeneously. For QCMD simulations, initial configurations with different numbers of water molecules were extracted from GCMC.…”
Section: Resultsmentioning
confidence: 99%
“…in so called sites I'). [31] It is worth noticing that the water fills the porous volume homogeneously. For QCMD simulations, initial configurations with different numbers of water molecules were extracted from GCMC.…”
Section: Resultsmentioning
confidence: 99%
“…The parameters are taken from Jaramillo et al [12] for the zeolite framework (in particular, Si and Al atoms are described as "T atoms" carrying identical charges) and from Dang et al [13] for Na + cations, together with the TIP4P water model of water [14]. This force field was successfully used in previous studies of water adsorption in Y and X zeolites [4,5,6,15,16]. Periodic boundary conditions are used, electrostatic interactions are computed using Ewald summation and a cut-off equal to half the box length is used to compute Lennard-Jones interactions.…”
Section: Monte Carlo Simulationsmentioning
confidence: 99%
“…One of the reasons for the discrepancy between cation location results is the strong sensitivity of cation distribution to experimental conditions (temperature, dehydration conditions, nature and quantity of sorbed molecules …) [1,3]. The presence of water has been shown to drastically modify the cation location in zeolites and in particular in faujasite zeolite [4,5,6,7,8]. The experimental determination of cation location in hydrated sample is complicated because of partial occupancies affecting low symmetry sites.…”
Section: Introductionmentioning
confidence: 99%
“…Therefore the use of these powerful methods must be restricted to the study of a limited number of molecular sieves in a limited number of temperature and adsorption conditions. However contrast powder diffraction analyses appear fully complementary with the work undertaken in the field of molecular simulations where significant advances have occurred in the codes and the potentials [39,40].…”
Section: Resultsmentioning
confidence: 99%