1997
DOI: 10.1039/a607528b
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Solid-state NMR study of locations and dynamics of interlayer cationsand water in kanemite

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Cited by 28 publications
(31 citation statements)
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“…In any case, these IR spectra clearly indicate that water in kanemite is much different than bulk water or ice, with low O-H bond stretching frequencies that are consistent with the solid state. The multiple peaks are consistent with the multiple forms of -O-H expected from the crystal structure, where the electron densities for silanol (Si-O-H) hydrogens and the O-H hydrogens of the water molecules directly coordinated to Na + are resolved, and at least two other types of water have been proposed [22,27]. Further detailed information must be obtained from the NMR analysis.…”
Section: Infrared Spectroscopysupporting
confidence: 64%
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“…In any case, these IR spectra clearly indicate that water in kanemite is much different than bulk water or ice, with low O-H bond stretching frequencies that are consistent with the solid state. The multiple peaks are consistent with the multiple forms of -O-H expected from the crystal structure, where the electron densities for silanol (Si-O-H) hydrogens and the O-H hydrogens of the water molecules directly coordinated to Na + are resolved, and at least two other types of water have been proposed [22,27]. Further detailed information must be obtained from the NMR analysis.…”
Section: Infrared Spectroscopysupporting
confidence: 64%
“…For comparison, the effective diameter of a water molecule is 0.28 nm and the diameter of a Na + ion is 0.19 nm [26]. X-ray crystallography and 23 Na solid state NMR of kanemite both show one Na + -binding site [22,27], but NMR studies of Zeolite A have shown variation in the location and coordination of Na + ions [28].…”
Section: X-ray Crystallography and Previous Nmr Resultsmentioning
confidence: 99%
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“…In the silicate layer of SKS-6, each tetrahedral silicon atom is bonded to three other tetrahedral silicon atoms via bridging oxygen atoms, leaving one coordination oxygen atom in a non-bridging form (having a negative charge) [5]. For kanemite, its crystal structure consists of alternating single layer sheets of SiO 4 tetrahedra [(SiO 3 ) 3 SiO À Na + ] or [(SiO 3 ) 3 SiOH] and hydrated sodium ions layer [23][24][25]. When SKS-6 is surrounded by water molecules, sodium ions bound to the non-bridging oxygen atoms will be attacked by water molecules and the framework SiO 4 tetrahedra will begin to hydrolyze, leading to the formation of kanemite phase.…”
Section: Article In Pressmentioning
confidence: 99%
“…[18][19][20] The local structures and dynamics of interlayer Na cations and water have also been studied by solid-state 1 H-, 29 Si-and 23 Na-NMR. 21 The interlayer water is present in two different states (bound as well as free) in kanemite, as revealed by quasi-elastic neutron scattering (QENS), thermogravimetry (TG) and 2 H-NMR measurements. 22 It has also been found by 2 H-NMR T 1 relaxation study that the hydrated water in kanemite is in the solid state (icelike) at room temperature.…”
Section: Layered Silicatesmentioning
confidence: 99%