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作者单位:G. D. Gatta (1) (2) G. Tabacchi (3) E. Fois (3) Y. Lee (4)
1. Dipartimento di Scienze della Terra, Università degli Studi di Milano, Via Botticelli 23, 20133, Milan, Italy 2. CNR - Istituto di Cristallografia, Sede di Bari, Via G. Amendola 122/o, Bari, Italy 3. Dipartimento di Scienza e Alta Tecnologia, Università degli Studi dell’Insubria, Via Valleggio 9, 22100, Como, Italy 4. Department of Earth System Sciences, Yonsei University, Seoul, 120749, Korea
刊物类别:Earth and Environmental Science
刊物主题:Earth sciences Mineralogy Crystallography Geochemistry Mineral Resources
出版者:Springer Berlin / Heidelberg
ISSN:1432-2021
文摘
The high-pressure behaviour and the P-induced structural evolution of a synthetic zeolite Rb7NaGa8Si12O40·3H2O (with edingtonite-type structure) were investigated both by in situ synchrotron powder diffraction (with a diamond anvil cell and the methanol:ethanol:water = 16:3:1 mixture as pressure-transmitting fluid) up to 3.27 GPa and by ab initio first-principles computational modelling. No evidence of phase transition or penetration of P-fluid molecules was observed within the P-range investigated. The isothermal equation of state was determined; V 0 and K T0 refined with a second-order Birch–Murnaghan equation of state are V 0 = 1311.3(2) Å3 and K T0 = 29.8(7) GPa. The main deformation mechanism (at the atomic scale) in response to the applied pressure is represented by the cooperative rotation of the secondary building units (SBU) about their chain axis (i.e. [001]). The direct consequence of SBU anti-rotation on the zeolitic channels parallel to [001] is the increase in pore ellipticity with pressure, in response to the extension of the major axis and to the contraction of the minor axis of the elliptical channel parallel to [001]. The effect of the applied pressure on the bonding configuration of the extra-framework content is only secondary. A comparison between the P-induced main deformation mechanisms observed in Rb7NaGa8Si12O40·3H2O and those previously found in natural fibrous zeolites is made.