1986
DOI: 10.1021/ja00268a002
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High-resolution aluminum-27 NMR of aluminosilicates

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Cited by 585 publications
(409 citation statements)
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“…Since Al atoms may be located in two distinct pore systems proposed for this zeolite, the presence of the two sets of signals derived from tetrahedral Al is understandable [34]. Lippmaa et al [35] showed that the chemical shifts of tetrahedral Al correlate with average Al-O-Si angles in zeolite frameworks and on this basis the average angles of 152 o and 164 o for the 55 and 48 ppm components were assigned. Keneddy et al [17] then assigned the presence of the 55 ppm peak to the population of T1, T3, T4, T5, T8 sites and the 48 ppm peak to T6 and T7 sites.…”
Section: Resultsmentioning
confidence: 95%
“…Since Al atoms may be located in two distinct pore systems proposed for this zeolite, the presence of the two sets of signals derived from tetrahedral Al is understandable [34]. Lippmaa et al [35] showed that the chemical shifts of tetrahedral Al correlate with average Al-O-Si angles in zeolite frameworks and on this basis the average angles of 152 o and 164 o for the 55 and 48 ppm components were assigned. Keneddy et al [17] then assigned the presence of the 55 ppm peak to the population of T1, T3, T4, T5, T8 sites and the 48 ppm peak to T6 and T7 sites.…”
Section: Resultsmentioning
confidence: 95%
“…This was done manually (using the diffractogram of an empty sample holder) in order to preserve any diffraction intensity from the amorphous content of the powders, however this introduces a small broad hump at lower angles due to differences in diffraction plane height between full and empty sample holders. [46,47], zeolites [48] and mullite [49]. Al(V) and Al(IV) are commonly observed in mullite-like structures in aluminosilicate glasses where charge balancing cations are not in excess [43], and as such any Al existing as Al(V) and Al(VI) in samples A and B is likely to provide some charge balancing to the negative charge associated with tetrahedral Al sites.…”
Section: X-ray Diffractionmentioning
confidence: 99%
“…Knowing the observed chemical shifts of the center of gravity of a peak in the two dimensions allows us to extract the isotropic chemical shift δ iso CS and the second-order quadrupole shift ω (2)iso −1/2 1/2 of the peak. These two parameters characterize the local symmetry of a crystallographic site in solids [94].…”
Section: Introductionmentioning
confidence: 99%