1998
DOI: 10.1016/s1386-1425(98)00035-3
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An FT-Raman study of solid-state ion exchange in zeolites

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Cited by 13 publications
(15 citation statements)
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“…The bands around 500 cm −1 are associated to zeolites with even-number rings [54], in this case W zeolite structure possess 8-member rings. The variation in the frequency of the bands is due to the nature of cations [55]. Additionally to these bands, in Fe-modified W zeolite new bands at 615 and 671 cm −1 were detected, they could be associated to the presence of the iron in the zeolite, considering that the only difference between the pristine and the modified zeolites is the chemical composition.…”
Section: Characterization Techniquesmentioning
confidence: 90%
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“…The bands around 500 cm −1 are associated to zeolites with even-number rings [54], in this case W zeolite structure possess 8-member rings. The variation in the frequency of the bands is due to the nature of cations [55]. Additionally to these bands, in Fe-modified W zeolite new bands at 615 and 671 cm −1 were detected, they could be associated to the presence of the iron in the zeolite, considering that the only difference between the pristine and the modified zeolites is the chemical composition.…”
Section: Characterization Techniquesmentioning
confidence: 90%
“…The Raman spectra (Figure 1b) of the pristine and the modified W zeolites shows the characteristic peaks of the zeolitic materials. The most intense bands correspond to the region of 300-600 cm −1 [54,55]. The band [54] at 295 cm −1 is associated to motion of an oxygen atom in a perpendicular plane to T-O-T bonds (T = Si or Al) while the bands at 414 and 423 cm −1 corresponding to vibration mode of tetrahedral in the network [56].…”
Section: Characterization Techniquesmentioning
confidence: 99%
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“…4 presents the Raman spectra of CrNaY support and the homologous catalysts prepared with the three different ligands. Although the spectra are dominated by the intrinsic background fluorescence of calcined zeolitic samples [38], it is possible to identify peaks at 1360 and 942 cm À1 in [CrL 1a ]NaY and [CrL 1b ]NaY. The spectrum of [CrL 1c ]NaY is similar to the one of CrNaY.…”
Section: Preparation and Characterization Of The Heterogeneous Cr-faumentioning
confidence: 94%
“…Vibrational spectroscopy is one of the most important experimental methods used in studies of zeolite structures [3][4][5][6][7][8][9][10]. It allows various frameworks to be identified and structural deformation to be specified using the envelope and integral intensities of bands in the pseudolattice region of the spectrum (linked to characteristic ring vibrations [11]).…”
Section: Introductionmentioning
confidence: 99%