The perturbation of water ‘sorbed’ in samples of zeolites of different structural type, genesis, and cation composition (K-, Na-, Mg- and Ca-rich zeolites), namely the CHA framework of a synthetic K-chabazite, the LTA framework of synthetic Na-A and Mg50-A zeolites, and the NAT framework of a natural scolecite, has been studied by FTIR-ATR spectroscopy, in the −10 to +80 ◦C temperature range. The aim was to show how differences in the chemical composition and/or in the topology of the zeolite framework and, in particular, the possibility for the guest water molecules to develop guest–guest and/or host– guest interactions, lead to substantial differences in their vibrational dynamical properties. The spectra, collected in the O–H stretching and H2O bending mode regions, are complex, with multiple bands being observed. As far as water in the CHA and LTA frameworks is concerned, whose behaviour is governed by the balance of water–water, water–framework and water–extra-framework cations interactions, the assignment of the resolved components of the O–H stretching band has been discussed by fitting the band shapes into individual components attributed to H2O molecules engaged in different degrees of hydrogen bonding. A detailed quantitative picture of the connectivity pattern of water, as a function of temperature and according to the chemical and topological properties of the environment, is furnished. The H2O bending vibrational bands give additional information that perfectly agrees with the results obtained from the analysis of the O–H stretching spectral region. In the case of scolecite, a small-pored zeolite where water–water interactions are eliminated, the increased complexity observed in the infrared spectra in the O–H stretching and H2O bending regions was explained as due to the hydrogen bonding between the water molecules and the network, and also with the extra-framework cation. Furthermore, these observations have been correlated with the different O· · ·O bond distances of the water molecules in the NAT framework.

Vibrational properties of water molecules adsorbed in different zeolitic frameworks

CRUPI, Vincenza;LONGO, FRANCESCA;MAJOLINO, Domenico;VENUTI, Valentina
2006-01-01

Abstract

The perturbation of water ‘sorbed’ in samples of zeolites of different structural type, genesis, and cation composition (K-, Na-, Mg- and Ca-rich zeolites), namely the CHA framework of a synthetic K-chabazite, the LTA framework of synthetic Na-A and Mg50-A zeolites, and the NAT framework of a natural scolecite, has been studied by FTIR-ATR spectroscopy, in the −10 to +80 ◦C temperature range. The aim was to show how differences in the chemical composition and/or in the topology of the zeolite framework and, in particular, the possibility for the guest water molecules to develop guest–guest and/or host– guest interactions, lead to substantial differences in their vibrational dynamical properties. The spectra, collected in the O–H stretching and H2O bending mode regions, are complex, with multiple bands being observed. As far as water in the CHA and LTA frameworks is concerned, whose behaviour is governed by the balance of water–water, water–framework and water–extra-framework cations interactions, the assignment of the resolved components of the O–H stretching band has been discussed by fitting the band shapes into individual components attributed to H2O molecules engaged in different degrees of hydrogen bonding. A detailed quantitative picture of the connectivity pattern of water, as a function of temperature and according to the chemical and topological properties of the environment, is furnished. The H2O bending vibrational bands give additional information that perfectly agrees with the results obtained from the analysis of the O–H stretching spectral region. In the case of scolecite, a small-pored zeolite where water–water interactions are eliminated, the increased complexity observed in the infrared spectra in the O–H stretching and H2O bending regions was explained as due to the hydrogen bonding between the water molecules and the network, and also with the extra-framework cation. Furthermore, these observations have been correlated with the different O· · ·O bond distances of the water molecules in the NAT framework.
2006
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11570/1704483
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