2009
DOI: 10.1016/j.clay.2008.07.028
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Characterization of GMZ bentonite and its application in the adsorption of Pb(II) from aqueous solutions

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Cited by 179 publications
(61 citation statements)
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“…That might be attributed to the greater selectivity of anionic sulfate groups of the resin for Na + cations than that for organic cations 23 since Na + ions are smaller in size in comparison to organic cations and hence the mobility of Na + is higher than organic cations 24 . Similar results represented by Wang 25 . For more explanation, the electrostatic interaction plays an essential role in the ion exchange technique.…”
Section: Effect Of Ionic Strengthsupporting
confidence: 77%
“…That might be attributed to the greater selectivity of anionic sulfate groups of the resin for Na + cations than that for organic cations 23 since Na + ions are smaller in size in comparison to organic cations and hence the mobility of Na + is higher than organic cations 24 . Similar results represented by Wang 25 . For more explanation, the electrostatic interaction plays an essential role in the ion exchange technique.…”
Section: Effect Of Ionic Strengthsupporting
confidence: 77%
“…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: 99%
“…As bandas na faixa de 3400-3500 cm -1 e 1642 cm -1 foram atribuídas ao modo de vibração de alongamento de água absorvida pelas argilas [3]. Absorção em torno de 1030 cm -1 foi referente ao estiramento Si-O da folha tetraédrica [26]. deformação angular do Si-O-Al e em torno de 464 cm -1 do Si-O-Si [27].…”
Section: Figura 2: Difratogramas De Raios X Das Amostras Arg1 (A) E Aunclassified