1998
DOI: 10.1016/s1387-1811(98)00053-5
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Structure analysis of mesoporous material ‘FSM-16’ Studies by electron microscopy and X-ray diffraction

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Cited by 52 publications
(34 citation statements)
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“…One possible explanation for the lower surface areas and pore volumes is that the pore walls of the Fe-FSM-16 samples prepared by M-H synthesis are thicker than the FSM-16 samples prepared by conventional-hydrothermal synthesis reported in the literature [3,4]. The X-ray powder diffraction patterns of the solids prepared by M-H synthesis showed three peaks indexed as (100), (110) and (200) reflections in the range of 2h = 2°-5°, which correspond to the wellordered hexagonal mesoporous structure.…”
Section: Xrd N 2 Adsorption Isotherms and Chemical Analysismentioning
confidence: 96%
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“…One possible explanation for the lower surface areas and pore volumes is that the pore walls of the Fe-FSM-16 samples prepared by M-H synthesis are thicker than the FSM-16 samples prepared by conventional-hydrothermal synthesis reported in the literature [3,4]. The X-ray powder diffraction patterns of the solids prepared by M-H synthesis showed three peaks indexed as (100), (110) and (200) reflections in the range of 2h = 2°-5°, which correspond to the wellordered hexagonal mesoporous structure.…”
Section: Xrd N 2 Adsorption Isotherms and Chemical Analysismentioning
confidence: 96%
“…The 57 Fe Mössbauer spectra of the samples were recorded between 298 and 4.2 K using a 2-GBq 57 Co/Rh source and a conventional constant acceleration spectrometer operated in triangular mode. Spectra at temperatures below 4.2 K were obtained in a 3 He- 4 He dilution refrigerator and in-field spectra with a superconducting coil. The applied magnetic field (H) was parallel to the c-ray direction of propagation.…”
Section: Characterization Techniquesmentioning
confidence: 99%
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“…Sakamoto et al concluded that FSM-16 and MCM-41 are structurally different. [88] By their detailed TEM observation of a 2D hexagonal product recovered in the initial stage of the formation of FSM-16, they stated that the 2D hexagonal phase may also be formed through fragmentation of the silicate sheets of kanemite. However, the presence of a layered intermediate and the fragmentation of the silicate sheets had not been detected by any experimental data at that time.…”
Section: On the Difference Between Fsm-16 And Mcm-41mentioning
confidence: 99%
“…However, the technique encounters difficulty in the analysis of pillared clay in which the pore structure is not cylindrical nor slit-like. Electron microscopy is known to a powerful tool for analysis of zeolite pores (6,7). A few studies of pillared clays have been carried out (8), but it is difficult to observe pillars shielded by silicate layers.…”
Section: Introductionmentioning
confidence: 99%