2008
DOI: 10.1016/j.physb.2008.04.008
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Preparation and characterization of montmorillonite–silica nanocomposites: A sol–gel approach to modifying clay surfaces

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Cited by 48 publications
(30 citation statements)
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“…Several characterization techniques were employed in order to identify the changes in clay: fourier transforminfra-red (FT-IR), X-ray diffraction (XRD), raman spectroscopy, Si/Al NMR, transmission electron microscopy (TEM), scanning electron microscopy (SEM), energy dispersive X-ray spectroscopy (EDX) and nitrogen adsorption-desorption isotherms [14]. FT-IR is a complementary method to X-ray diffraction (XRD) and other methods used to investigate clays and clay minerals.…”
Section: Introductionmentioning
confidence: 99%
“…Several characterization techniques were employed in order to identify the changes in clay: fourier transforminfra-red (FT-IR), X-ray diffraction (XRD), raman spectroscopy, Si/Al NMR, transmission electron microscopy (TEM), scanning electron microscopy (SEM), energy dispersive X-ray spectroscopy (EDX) and nitrogen adsorption-desorption isotherms [14]. FT-IR is a complementary method to X-ray diffraction (XRD) and other methods used to investigate clays and clay minerals.…”
Section: Introductionmentioning
confidence: 99%
“…The most widely used method is the treatment of the clays with quaternary ammonium salts, which allows the substitution of some metal ions present in the structures of the clay by quaternary ammonium ions with large organic groups. Another modification procedure includes the grafting of silanes [10,11]. Clay minerals have reactive hydroxyl groups that can react with silanol (Si-OH) groups of the hydrolyzed silane to form siloxane (Si-O-Si) bonds.…”
Section: Introductionmentioning
confidence: 99%
“…Clay minerals have reactive hydroxyl groups that can react with silanol (Si-OH) groups of the hydrolyzed silane to form siloxane (Si-O-Si) bonds. A discussion on the location of the reactive -OH groups in the clay crystals, mainly in the edges and the structural defects of the crystals, can be found in the literature [9][10][11][12][13][14]. When the silanization occurs in the interlayer of the clay, the distance between the layers increases, thus favoring the compounding of the nanocomposites [13].…”
Section: Introductionmentioning
confidence: 99%
“…This may be because TEOS molecules are smaller than those of KH550 and become more accessible to attached to the kaolinite surface more easily. Some of the hydroxyl groups in the hydrolyzed TEOS could react with hydroxyl groups located present on the kaolinite surface, and others could interact with hydroxyl groups in the silane coupling agent, and form a large network (Qian, Hu, Zhang, & Yang, 2008). The bands at 3694.8 and 3621.4 cm −1 are ascribed to the outer hydroxyl groups and inner hydroxyl groups, respectively, of kaolinite.…”
Section: Resultsmentioning
confidence: 99%