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Cation Exchange, Dehydration, and Calcination in Clinoptilolite:  In Situ X-ray Diffraction and Computer Modeling

Matthew N. JohnsonBirkbeck, University of LondonD. O'ConnorDaresbury LaboratoryP. BarnesBirkbeck, University of LondonC. Richard A. CatlowBirkbeck, University of LondonScott L. OwensThe Royal Institution, 21 Albemarle Street, London W1X 4BS, United Kingdom, Department of Crystallography, Birkbeck College, Malet Street, London WC1 E 7HX, United Kingdom, BNFL, Risley, Warrington, Cheshire WA3 6AS, United Kingdom, and CLRC Daresbury Laboratory, Daresbury, Warrington WA4 4AD, United KingdomGopinathan SankarDaresbury LaboratoryRobert G. BellThe Royal Institution, 21 Albemarle Street, London W1X 4BS, United Kingdom, Department of Crystallography, Birkbeck College, Malet Street, London WC1 E 7HX, United Kingdom, BNFL, Risley, Warrington, Cheshire WA3 6AS, United Kingdom, and CLRC Daresbury Laboratory, Daresbury, Warrington WA4 4AD, United KingdomSimon J. TeatBirkbeck, University of LondonRichard A. StephensonBirkbeck, University of London
2003en

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Clinoptilolite is a natural microporous material possessing a versatile range of cation exchange properties that are exploited in many industrial processes. The dehydration and cation mobility of three prototype forms, Cs−, K−, and Na−clinoptilolite, have been studied using in situ synchrotron energy dispersive and microcrystal diffraction with a novel hybrid simulation technique. This exposes the different responses of the framework, cation, and water components to dehydration processes. The responses are illustrated for the Cs and Na forms using structural snapshots and statistically averaged parameters. The “heat collapse” framework transformation has been identified with the pure Na form by both the in situ diffraction data and the computer modeling.

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