2008
DOI: 10.1016/j.jhazmat.2007.06.040
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An investigation of Cu(II) adsorption by raw and acid-activated bentonite: A combined potentiometric, thermodynamic, XRD, IR, DTA study

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Cited by 206 publications
(96 citation statements)
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“…The clays-Cu interactions occurred spontaneously and were accompanied by a decrease in Gibbs free energy (ΔG < 0). The degree of spontaneity was found to decline as the process temperature rose, ranging from −16.6 to −27.9 kJ.mol -1 for the temperature range between 273 and 348 K. Adsorption and ion exchange of Cu(II) on different clays had already been reported as endothermic [23][24][25][26][27][28] , as shown in Table 6. It was likely that adsorption of Cu(II) ions on clay surface require an activation energy and rise in temperature helped more Cu(II) ions to overcome this energy barrier and get attached to the surface 23 .…”
Section: Adsorption Thermodynamicsmentioning
confidence: 90%
“…The clays-Cu interactions occurred spontaneously and were accompanied by a decrease in Gibbs free energy (ΔG < 0). The degree of spontaneity was found to decline as the process temperature rose, ranging from −16.6 to −27.9 kJ.mol -1 for the temperature range between 273 and 348 K. Adsorption and ion exchange of Cu(II) on different clays had already been reported as endothermic [23][24][25][26][27][28] , as shown in Table 6. It was likely that adsorption of Cu(II) ions on clay surface require an activation energy and rise in temperature helped more Cu(II) ions to overcome this energy barrier and get attached to the surface 23 .…”
Section: Adsorption Thermodynamicsmentioning
confidence: 90%
“…3. The absorption band at 3621 cm −1 was due to the stretching vibration of structural OH group (Al-OH) of Na + -bentonite; the bands at 3432 and 1631 cm −1 corresponded to the stretching and bending vibrations of H 2 O, respectively; the band at 1045 cm −1 represented the stretching vibration of Si-O, while the band corresponding to Al-Al-OH bending vibration was observed at 921 cm −1 ; the band at 790 cm −1 implied quartz admixture in the samples; the bands at 528 and 466 cm −1 were associated with the bending vibrations of Si-O-Mg and Si-O-Fe, respectively (Eren and Afsin, 2008;Liu et al, 2010;Wang et al, 2009;Yuan et al, 2008). After clay was pillared, the amount of OH groups (H-OH and Al-OH) increased markedly on account of the much stronger absorption at 1631, 3432 and 3621 cm −1 .…”
Section: Resultsmentioning
confidence: 97%
“…All FTIR spectra showed the presence of similar peaks in the range of 1100-600 cm -1 . In this range, there are peaks related to stretching vibration of Si-O groups, Al-O-Si and Si-O-Si bending vibrations and Al-O and Si-O out of plane vibrations of bentonite framework structure [24]. Thus, these FTIR spectra show the structural stability of bentonite after modification with Ag and CTAB [17].…”
Section: Antibacterial Assaymentioning
confidence: 85%
“…The XRD patterns shows that the major phase is montmorillonite (M) and other minor phases present in the sample are illite (I), quartz (Q) and kaolinite (K) [23]. There were no changes in the XRD patterns of both samples indicating that the structure of bentonite was stable after loaded with Ag cations [24]. Characterizations of both samples were further performed by elemental analysis qualitatively using EDX (Fig.…”
Section: Antibacterial Assaymentioning
confidence: 99%