1976
DOI: 10.1139/v76-084
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Abstract: As with other silicas and aluminas, it is shown that a broad general fluorescence from Y zeolite samples excited by irradiation with the 6328 Å line of a He/Ne laser can be greatly reduced by heating the zeolite in oxygen at 500 °C. This general fluorescence is attributed to the presence of traces of unsaturated hydrocarbon impurities which can be burned off by the oxygen treatment. A narrower residual fluorescence in the region of 14 000–14 500 cm−1 is attributed to the presence of Fe3+ impurities.Successful … Show more

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Cited by 34 publications
(13 citation statements)
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(23 reference statements)
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“…Egerton et a1. 6 also observed a shift of the same order of magnitude of the v1 mode of pyridine adsorbed onto faujasites, though they did not give an explanation for this phenomenon. As the effect is much smaller for the v12 than for the uI mode, we will not discuss the former band in detail.…”
Section: Resultsmentioning
confidence: 91%
“…Egerton et a1. 6 also observed a shift of the same order of magnitude of the v1 mode of pyridine adsorbed onto faujasites, though they did not give an explanation for this phenomenon. As the effect is much smaller for the v12 than for the uI mode, we will not discuss the former band in detail.…”
Section: Resultsmentioning
confidence: 91%
“…However, these data do not provide information about the location of active sites in the zeolite crystals. In a similar way to FTIR spectroscopy, the interactions of pyridine with different types of acid sites can be distinguished using the strong resonances of the ring breathing modes (900-1100 cm −1 ) in Raman spectroscopy [41][42][43][44]. The influence of different types of interactions on the ring breathing modes of pyridine can be illustrated with the Raman spectra of the molecule in different solutions ( Figure S4).…”
Section: Resultsmentioning
confidence: 99%
“…After the initial removal of excess solvent, there was already a strong peak at 418 cm −1 , consistent with PS 4 3− units, possibly complexed with solvent [24] . There are also two fairly strong peaks at 1003 cm −1 and 1034 cm −1 ; this is not representative of free pyridine (ν 1 and ν 12 at 991 cm −1 and 1030 cm −1 ) but rather pyridine complexed to Li + cations, for instance in zeolites (1002 cm −1 and 1036 cm −1 ) [25] . This result suggests that, despite being immersed in excess ACN, pyridine molecules originally bound to the phosphorus atoms of P 2 S 5 remain preferentially complexed to the material even after reaction (though likely now complexed to Li + , as demonstrated by Schönberger and coworkers with py 8 Li 4 P 2 S 6 ) [26] .…”
Section: Figurementioning
confidence: 93%