2019
DOI: 10.3390/min9100626
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The Removal of Uranium and Thorium from Their Aqueous Solutions by 8-Hydroxyquinoline Immobilized Bentonite

Abstract: The sorption of uranium and thorium from their aqueous solutions by using 8-hydroxyquinoline modified Na-bentonite (HQ-bentonite) was investigated by the batch technique. Na-bentonite and HQ-bentonite were characterized by X-ray fluorescence (XRF), X-ray diffraction (XRD), scanning electron microscopy (SEM), and Fourier Transform Infrared (FTIR) spectroscopy. Factors that influence the sorption of uranium and thorium onto HQ-bentonite such as solution pH, contact time, initial metal ions concentration, HQ-bent… Show more

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Cited by 34 publications
(9 citation statements)
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“…The BT powder showed an initial basal spacing ( d 001 ) of 12.2 Å and several characteristic diffraction peaks of montmorillonite at 7°, 20°, 29°, 35°, and quartz at 27°. [ 41 ] The BT crystals in all the WiSCEs possessed the same d 001 of 18.9 Å after water intercalation, corresponding to an enlarged interlayer spacing from 2.6 to 9.3 Å (Figure S8, Supporting Information). [ 42 ] This is in good agreement with the phenomenon observed in prior work, in which the swelling of BT crystals reached equilibrium with a d 001 of ≈19.0 Å when the water content exceeded the threshold of 28.6 wt.%.…”
Section: Resultsmentioning
confidence: 99%
“…The BT powder showed an initial basal spacing ( d 001 ) of 12.2 Å and several characteristic diffraction peaks of montmorillonite at 7°, 20°, 29°, 35°, and quartz at 27°. [ 41 ] The BT crystals in all the WiSCEs possessed the same d 001 of 18.9 Å after water intercalation, corresponding to an enlarged interlayer spacing from 2.6 to 9.3 Å (Figure S8, Supporting Information). [ 42 ] This is in good agreement with the phenomenon observed in prior work, in which the swelling of BT crystals reached equilibrium with a d 001 of ≈19.0 Å when the water content exceeded the threshold of 28.6 wt.%.…”
Section: Resultsmentioning
confidence: 99%
“…The band at 1428.18 cm −1 corresponds to the bending vibration of the Al-OH and Si-OH bonds in the octahedral and tetrahedral sheets of the bentonite structure. The absorption bands between 3392.58 cm −1 could be ascribed to stretching vibrations of structural OH-stretching vibrations that have Al and Mg coordination groups with octahedral layer of montmorillonite and water [45]. The broad infrared spectroscopy bond-stretching peak between 3693.93 and 1630.21 cm −1 wave numbers (Fig.…”
Section: Ft-ir Spectroscopymentioning
confidence: 96%
“…The existence of interlayer water in the WiSCEs was evidenced by X-ray diffraction (XRD) tests, as shown in Figure 2b. The BT powder showed an initial basal spacing (d001) of 12.2 Å and several characteristic diffraction peaks of montmorillonite at 7 °, 20 °, 29 °, 35 ° and quartz at 27 ° [49].…”
Section: Electrolyte Properties and Structuresmentioning
confidence: 99%