Elementary Steps of Faujasite Formation Followed by in Situ Spectroscopy

Ex situ and in situ spectroscopy was used to identify the kinetics of processes during the formation of the faujasite (FAU) zeolite lattice from a hydrous gel. Using solid-state 27Al magic angle spinning (MAS) nuclear magnetic resonance (NMR), the autocatalytic transformation from the amorphous gel...

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Published inChemistry of materials Vol. 30; no. 3; pp. 888 - 897
Main Authors Prodinger, Sebastian, Vjunov, Aleksei, Hu, Jian Zhi, Fulton, John L, Camaioni, Donald M, Derewinski, Miroslaw A, Lercher, Johannes A
Format Journal Article
LanguageEnglish
Published United States American Chemical Society 13.02.2018
American Chemical Society (ACS)
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Abstract Ex situ and in situ spectroscopy was used to identify the kinetics of processes during the formation of the faujasite (FAU) zeolite lattice from a hydrous gel. Using solid-state 27Al magic angle spinning (MAS) nuclear magnetic resonance (NMR), the autocatalytic transformation from the amorphous gel into the crystalline material was monitored. Al X-ray absorption near-edge structure shows that most Al already adopts a tetrahedral coordination in the X-ray-amorphous aluminosilicate at the beginning of the induction period, which hardly changes throughout the rest of the synthesis. Using 23Na NMR spectroscopy, environments in the growing zeolite crystal were identified and used to define the processes in the stepwise formation of the zeolite lattice. The end of the induction period was accompanied by a narrowing of the 27Al and 23Na MAS NMR peak widths, indicating the increased level of long-range order. The experiments show conclusively that the formation of faujasite occurs via the continuous formation and subsequent condensation of intermediary sodalite-like units that constitute the key building block of the zeolite.
AbstractList Ex situ and in situ spectroscopy was used to identify the kinetics of processes during the formation of the faujasite (FAU) zeolite lattice from a hydrous gel. Using solid-state 27Al magic angle spinning (MAS) nuclear magnetic resonance (NMR), the autocatalytic transformation from the amorphous gel into the crystalline material was monitored. Al X-ray absorption near-edge structure shows that most Al already adopts a tetrahedral coordination in the X-ray-amorphous aluminosilicate at the beginning of the induction period, which hardly changes throughout the rest of the synthesis. Using 23Na NMR spectroscopy, environments in the growing zeolite crystal were identified and used to define the processes in the stepwise formation of the zeolite lattice. The end of the induction period was accompanied by a narrowing of the 27Al and 23Na MAS NMR peak widths, indicating the increased level of long-range order. The experiments show conclusively that the formation of faujasite occurs via the continuous formation and subsequent condensation of intermediary sodalite-like units that constitute the key building block of the zeolite.
Ex situ and in situ spectroscopy was used to identify the kinetics of processes during the formation of the faujasite (FAU) zeolite lattice from a hydrous gel. Using solid-state 27Al MAS NMR, the autocatalytic transformation from the amorphous gel into the crystalline material was monitored. Al-XANES shows that most Al already adopts a tetrahedral coordination in the X-ray-amorphous aluminosilicate at the beginning of the induction period, which hardly changes throughout the rest of the synthesis. Using 23Na NMR spectroscopy, environments in the growing zeolite crystal were identified and used to define the processes in the stepwise formation of the zeolite lattice. The end of the induction period was accompanied by a narrowing of the 27Al and 23Na MAS NMR peak widths, indicating the increased long-range order. The experiments show conclusively that the formation of faujasite occurs via the continuous formation and subsequent condensation of intermediary sodalite-like units that constitute the key building block of the zeolite. Acknowledgement The authors thank T. Huthwelker for assistance with XAFS experiment setup at the Swiss Light Source (PSI, Switzerland). Further, we would like to acknowledge V. Shutthanandan and B.W. Arey for performing Helium ion microscopy as well as Z. Zhao, N.R. Jaeger, M. Weng, C. Wan and M. Hu for aiding in the NMR experimental procedure. T. Varga is acknowledged for his help with the capillary XRD. A.V., D.M.C., J.H., J.L.F and J.A.L. were supported by the US Department of Energy, Office of Science, Office of Basic Energy Sciences. S.P. and M.A.D. acknowledge support by the Materials Synthesis and Simulation Across Scales (MS3 Initiative) conducted under Laboratory Directed Research & Development Program at PNNL. The in situ NMR experiments were supported by the U. S. Department of Energy (DOE), Office of Science, Office of Basic Energy Sciences, Division of Chemical Sciences, Biosciences and Geosciences. Part of the research described in this paper was performed in the Environmental Molecular Sciences Laboratory (EMSL), a national scientific user facility sponsored by the DOE’s Office of Biological and Environmental Research and located at Pacific Northwest National Laboratory (PNNL). PNNL is operated for the US DOE by Battelle.
Author Lercher, Johannes A
Prodinger, Sebastian
Derewinski, Miroslaw A
Fulton, John L
Camaioni, Donald M
Hu, Jian Zhi
Vjunov, Aleksei
AuthorAffiliation TU München
Institute for Integrated Catalysis
Department of Chemistry and Catalysis Research Institute
Pacific Northwest National Laboratory
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Snippet Ex situ and in situ spectroscopy was used to identify the kinetics of processes during the formation of the faujasite (FAU) zeolite lattice from a hydrous gel....
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SubjectTerms faujasite
in situ characterization
solid-state NMR
x-ray absorption spectroscopy
zeolite synthesis
Title Elementary Steps of Faujasite Formation Followed by in Situ Spectroscopy
URI http://dx.doi.org/10.1021/acs.chemmater.7b04554
https://www.osti.gov/biblio/1430418
Volume 30
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