2017
DOI: 10.14233/ajchem.2017.20252
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Synthesis and Characterization of New Tin(IV) Iodophosphosilicate Cation Exchanger

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“…Infrared spectra of zeolites in the 1300-400 cm −1 region generally consist of two vibration classes: (i) originating from the internal vibration of the TO 4 tetrahedron framework, which are the primary structural units in zeolite frameworks, and (ii) vibrations arising from the external connection between tetrahedral units sensitive to the framework structure and the presence of secondary structural units, the building blocks of polyhedral such as rings and pores. Characteristic FTIR bands of zeolites are given in Table 7 (Suresh Kumar 2007).…”
Section: Ft-ir Analysismentioning
confidence: 99%
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“…Infrared spectra of zeolites in the 1300-400 cm −1 region generally consist of two vibration classes: (i) originating from the internal vibration of the TO 4 tetrahedron framework, which are the primary structural units in zeolite frameworks, and (ii) vibrations arising from the external connection between tetrahedral units sensitive to the framework structure and the presence of secondary structural units, the building blocks of polyhedral such as rings and pores. Characteristic FTIR bands of zeolites are given in Table 7 (Suresh Kumar 2007).…”
Section: Ft-ir Analysismentioning
confidence: 99%
“…Symmetric stretching modes in the lower spectral region of 720-650 cm −1 shift to the higher region of 820-750 cm −1 with the inclusion of a tetrahedral stretch. The weak absorption bands at 650 cm −1 are due to the interaction between the alumina tetrahedra and Al 3+ in the zeolite structure, and the splitting state of the peak in this region indicates that there is high O-Si-O in the structure (Suresh Kumar 2007;Tabassum et al 2018).…”
Section: Ft-ir Analysismentioning
confidence: 99%
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