2017
DOI: 10.1002/ange.201602856
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On Layered Silicates and Zeolitic Nanosheets

Abstract: Supportinginformation and the ORCID identification number(s) for the author(s) of this article can be found under: http://dx.

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Cited by 2 publications
(5 citation statements)
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“…[4,5] These displacements in the 29 Si signals establish that the local bonding environments of the nanolayered silicates are transforming and, as they do so,a re correlated with Q 42 9 Si signals (pink band in Figure 1a)t hat are in the spectral region À110 to À114 ppm of MFI zeolite frameworks that is distinct from any of the Q 4 nanolayered silicate signals (specifically sites 4and 5 at À108.8 and À114.9 ppm). Thed isplaced signals are associated with regions of the nanolayered silicate frameworks that are rearranging to form mesostructured MFI zeolite frameworks,consistent with the 2D J-mediated NMR and electron microscopy results discussed below.Dissolution and recrystallization would produce physical mixtures of macroscopically separated nanolayered silicate and MFI zeolite species that would generally be distant from each other and result in negligible correlated intensity in the 2D 29 Si{ 29 Si}NMR spectra, contrary to the assertion by Goesten, et al [26] that such commingled phases would be "apt to magnetization transfer in the 2D NMR experiment. "…”
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confidence: 80%
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“…[4,5] These displacements in the 29 Si signals establish that the local bonding environments of the nanolayered silicates are transforming and, as they do so,a re correlated with Q 42 9 Si signals (pink band in Figure 1a)t hat are in the spectral region À110 to À114 ppm of MFI zeolite frameworks that is distinct from any of the Q 4 nanolayered silicate signals (specifically sites 4and 5 at À108.8 and À114.9 ppm). Thed isplaced signals are associated with regions of the nanolayered silicate frameworks that are rearranging to form mesostructured MFI zeolite frameworks,consistent with the 2D J-mediated NMR and electron microscopy results discussed below.Dissolution and recrystallization would produce physical mixtures of macroscopically separated nanolayered silicate and MFI zeolite species that would generally be distant from each other and result in negligible correlated intensity in the 2D 29 Si{ 29 Si}NMR spectra, contrary to the assertion by Goesten, et al [26] that such commingled phases would be "apt to magnetization transfer in the 2D NMR experiment. "…”
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confidence: 80%
“…If the MFI zeolite frameworks formed only through dissolution and reprecipitation, as suggested by Goesten, et al, [26] the nanolayered silicate and MFI zeolite moieties would not be covalently bonded to any significant extent. The presence of the J-mediated 29 Si signals in Figure 1b is instead consistent with the non-topotactic rearrangement of nanolayered silicates to form the MFI zeolite frameworks.T he regions over which such transformations occur are sufficiently numerous and large that they can be resolved in the representative TEM image shown in Figure 4b of Messinger, et al, [1] which we have modified in Figure 1c to emphasize aregion in which nanolayered silicate species are rearranging into mesostructured MFI zeolite nanosheets (red box in Figure 1c).…”
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confidence: 95%
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“…The investigation of zeolite self-assembly and crystallization presents a persisting challenge. 26 It is generally accepted that weak and strong interactions between template and building units lead to the formation of aluminosilicate framework around structuredirecting agents (SDAs). The mechanism of zeolite formation is commonly studied in colloidal precursor suspensions permitting the growth process to be followed with a number of noninvasive techniques.…”
Section: ■ Introductionmentioning
confidence: 99%