1998
DOI: 10.1016/s1387-1811(97)00013-9
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Thermal and cation influence on ir vibrations of modified natural clinoptilolite

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1998
1998
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Cited by 52 publications
(24 citation statements)
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“…The relative intensity of some zeolite bands changed moderately after HT, which can be associated with the ion exchange process. The changes observed in the relative transmittance of the 1205 and 456 cm−1 vibration bands are the same as reported by Rodríguez et al [15] for this zeolite as a consequence of the partial exchange of Ca2+ by Na+ in NZ. These results agree well with those obtained via XRD.…”
Section: Methodssupporting
confidence: 89%
“…The relative intensity of some zeolite bands changed moderately after HT, which can be associated with the ion exchange process. The changes observed in the relative transmittance of the 1205 and 456 cm−1 vibration bands are the same as reported by Rodríguez et al [15] for this zeolite as a consequence of the partial exchange of Ca2+ by Na+ in NZ. These results agree well with those obtained via XRD.…”
Section: Methodssupporting
confidence: 89%
“…The strongest band observed at ca. 1055 cm Ϫ1 was assigned to asymmetric stretching of the external tetrahedral linkages (Rodriguez-Fuentes et al 1998). The second strongest band at ca.…”
Section: Ft-ir Analysismentioning
confidence: 99%
“…A comparison of the spectra of all the samples showed that there were no significant differences between them. Peaks at 1060 cm Ϫ1 , 790 cm Ϫ1 and 609 cm Ϫ1 were characteristic of clinoptilolite (Çaglar et al 2007;Rodriguez-Fuentes et al 1998). The strongest band observed at ca.…”
Section: Ft-ir Analysismentioning
confidence: 99%
“…It is reported that IR bands in the 420-500 cm -1 region and those between 520 and 600 cm -1 are assigned to internal tetrahedron vibrations such as 6-and 5-rings of T-O-T (T = Si or Al) in zeolites [28]. These IR bands for clinoptilolite and zeolite-P were observed between 430 and 604 cm -1 [29,30].…”
Section: Structural Parametersmentioning
confidence: 99%