2019
DOI: 10.1007/s10853-019-03407-w
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Analysis of theoretical and experimental X-ray diffraction patterns for distinct mordenite frameworks

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Cited by 17 publications
(8 citation statements)
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“…The characteristic peaks can be observed at 2θ = 13.4°, 15.3°, 19.7°, 22.3°, 25.7°, 26.4°, 27.8°, 31.0°, and 35.8°, which are associated with MOR, the Miller indices corresponding to these peaks are also marked [38]. Compared with H-MOR, the peak intensities of Ag-MOR at 19.7°, 22.3° and 25.7° are drastically attenuated, which was also found in other research [40]. These results indicate that MOR was sensitive to the addition of Ag during the ion exchange.…”
Section: Introductionsupporting
confidence: 79%
“…The characteristic peaks can be observed at 2θ = 13.4°, 15.3°, 19.7°, 22.3°, 25.7°, 26.4°, 27.8°, 31.0°, and 35.8°, which are associated with MOR, the Miller indices corresponding to these peaks are also marked [38]. Compared with H-MOR, the peak intensities of Ag-MOR at 19.7°, 22.3° and 25.7° are drastically attenuated, which was also found in other research [40]. These results indicate that MOR was sensitive to the addition of Ag during the ion exchange.…”
Section: Introductionsupporting
confidence: 79%
“…This indicates that Cu 2+ ions occupy similar cationic positions in the channels of mordenite, regardless of the exchange method used. A more detailed study of the structure is undoubtedly of interest, as it would provide valuable information on the local structure rearrangement caused by ion-exchange procedure, as it was observed in Ag- and Fe-exchanged mordenite [31], and its results will be published elsewhere.…”
Section: Discussionmentioning
confidence: 99%
“…However, the variations of the relative intensities of several peaks were sensitive to Ag + and Zn 2+ incorporation, in particular the planes (111) at 6.3°, (220) at 10.3°, (311) at 12.1°, and (331) at 15.9° labeled with “@” (see Figure ). As reported previously, the relative intensity changes in the diffraction peaks of zeolite after the ion exchange process, especially with transition metals, are mainly associated with the changes in the local structure (exchange sites) of the zeolite. The latter allowed us to conclude the preferential location of the different metal cations.…”
Section: Resultsmentioning
confidence: 95%
“…The latter allowed us to conclude the preferential location of the different metal cations. Also, the variation in the intensity is strongly influenced by the metal charge on the support . Despite the light changes in the local structure, it may be concluded that the zeolite structure remains stable after ion exchange with Ag + and Zn 2+ cations because neither additional peaks nor any shift of characteristic signals was observed in the diffractograms.…”
Section: Resultsmentioning
confidence: 99%