2012
DOI: 10.1016/j.saa.2012.07.085
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FTIR spectroscopy study of the structure changes of palygorskite under heating

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Cited by 205 publications
(83 citation statements)
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“…1). There is also a gradual decrease in the intensity of the band at 3,200-3,800 cm −1 which is associated with OH stretching of water coordinated to Al, Mg and zeolitic water [12], although the band intensity slightly increased at 473.15 K because of the re-adsorption of water during the experimental procedure as has been reported by other researchers [13] Table 3 shows the variation of specific surface, external surface area, pore volume and pore size with calcination temperature. The external surface area was calculated from the PSD generated by laser diffraction by first transforming the volume distribution to a number density distribution and then using the method of moments to calculate the second moment (m 2 equivalent to external surface area) [17].…”
Section: June 2011supporting
confidence: 74%
“…1). There is also a gradual decrease in the intensity of the band at 3,200-3,800 cm −1 which is associated with OH stretching of water coordinated to Al, Mg and zeolitic water [12], although the band intensity slightly increased at 473.15 K because of the re-adsorption of water during the experimental procedure as has been reported by other researchers [13] Table 3 shows the variation of specific surface, external surface area, pore volume and pore size with calcination temperature. The external surface area was calculated from the PSD generated by laser diffraction by first transforming the volume distribution to a number density distribution and then using the method of moments to calculate the second moment (m 2 equivalent to external surface area) [17].…”
Section: June 2011supporting
confidence: 74%
“…Sharp peak at 1039 cm −1 and 541 cm −1 belonged to the stretching of Si-O-Si bond in palygorskite tetrahedral sheet, which in parallel with peak at 467 cm −1 were designated to the bending of O-Si-O bonds (Fig. 7) [22]. Peak at 3698 cm −1 was due to the vibration of -OH in Mg-OH, while the vibration and bending of water molecules (coordinated or zeolitic) appeared at 3450 and 1654 cm −1 , respectively (Fig.…”
Section: Fourier Transforms Infrared Spectroscopy (Ftir)mentioning
confidence: 98%
“…Each ribbon is connected to the next by the inversion of SiO4 tetrahedron along the oxygen atom. This kind of arrangement makes the tetrahedrons continuously bonded via the ribbons, thereby composing of ribbons of phyllosilicate [7][8][9]. From the cross section vertical to the c-axis, the octahedron is sandwiched by two tetrahedron layer units to constitute the layer-ribbon units, forming zeolite-like channels with a size of about 0.38 nm×0.63 nm via the alternate arrangement of layer-ribbon units and channel units [10,11].…”
Section: Introductionmentioning
confidence: 99%