2019
DOI: 10.1016/j.clay.2019.105142
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Tamoxifen/montmorillonite system – Effect of the experimental conditions

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Cited by 16 publications
(8 citation statements)
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“…After the addition of MMT to CS, the diffraction was found at 14.40° (2θ). In agreement with previous studies [48, 52], the initial band intensity in CS was much broader compared to that of CS‐MMT, suggesting the amorphous nature of silica sheets in MMT. The band shift from a higher diffraction angle (20.14°) to a lower diffraction angle (14.40°) decreased the band intensity of CS‐MMT compared to CS.…”
Section: Resultssupporting
confidence: 92%
“…After the addition of MMT to CS, the diffraction was found at 14.40° (2θ). In agreement with previous studies [48, 52], the initial band intensity in CS was much broader compared to that of CS‐MMT, suggesting the amorphous nature of silica sheets in MMT. The band shift from a higher diffraction angle (20.14°) to a lower diffraction angle (14.40°) decreased the band intensity of CS‐MMT compared to CS.…”
Section: Resultssupporting
confidence: 92%
“…This saturation is because of the high initial adsorption of RIF molecules by the adsorbent because, in shorter contact times, rapid competition for active sites leads to a decrease in the amount of active sites available. 77 As previously discussed, the way the molecule is found in the medium (neutral, cationic, or anionic) depends on the pH and, consequently, the characteristics of the adsorption process are affected. Therefore, as RIF has its totality in its cationic form at pH 2, it showed high incorporation efficiency values (almost 100%).…”
Section: ■ Results and Discussionmentioning
confidence: 47%
“…The system is in equilibrium after 180 min, and saturation can be observed in longer contact times, which results in a slower adsorption process. This saturation is because of the high initial adsorption of RIF molecules by the adsorbent because, in shorter contact times, rapid competition for active sites leads to a decrease in the amount of active sites available …”
Section: Resultsmentioning
confidence: 99%
“…The three clay minerals exhibited characteristic bands in similar regions and were differentiated by the intensities and bandwidths in the main areas that characterize the materials. These areas are related to tetrahedral sheets Si-O-Si (950–1250 cm −1 ) and M-OH octahedral (M indicates a metal, e.g., Al–Al–OH, Mg–Mg–OH, Al–Fe–OH) that appear in the low-wavelength region as well as bands attributed to hydroxyls and water molecules that appear between 3200–3440 cm −1 and 1650 cm −1 , respectively [22,24,32,34,35,36,37,38,39].…”
Section: Resultsmentioning
confidence: 99%