Issue 22, 2000

Understanding negative thermal expansion and ‘trap door’ cation relocations in zeolite rho

Abstract

In situ time-resolved synchrotron X-ray and neutron powder diffraction studies indicate that the negative thermal expansion and ‘trap door’ cation relocations observed in zeolite rho result from water-mediated chemical changes that occur during dehydration.

Article information

Article type
Communication
Submitted
18 Aug 2000
Accepted
03 Oct 2000
First published
31 Oct 2000

Chem. Commun., 2000, 2221-2222

Understanding negative thermal expansion and ‘trap door’ cation relocations in zeolite rho

B. A. Reisner, Y. Lee, J. C. Hanson, G. A. Jones, J. B. Parise, D. R. Corbin, B. H. Toby, A. Freitag, J. Z. Larese and V. Kahlenberg, Chem. Commun., 2000, 2221 DOI: 10.1039/B006929I

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