2016
DOI: 10.1016/j.clay.2016.05.021
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Investigating the expanding behavior and thermal stability of HDPy modified organo-bentonite by X-ray diffraction technique

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Cited by 7 publications
(4 citation statements)
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“…The value corresponding to this peak belongs to the distance between the two layers, giving the basal space calculated by Bragg's equations 49 at 12.04 nm. Another prominent peak is at the 28.5°, the peak of the (003) surface of montmorillonite, as reported by Orucoglu et al 50 As also seen in the preattritor Na-MMT curve (Figure 5g), along with prominent montmorillonite peaks, Illite was found at around 8.8°, clinoptilolite at 10.2°, and quartz, calcite, and dolomite minerals at 27, 28.5, and 29.5°, respectively. Similar findings were obtained from the same samples previously studied by Bulut et al, Orucoglu et al, and O ̈nal et al 48,50,51 However, it is quite difficult to make these inferences from the XRD pattern of postattritor nano-MMT.…”
Section: Ee%supporting
confidence: 82%
“…The value corresponding to this peak belongs to the distance between the two layers, giving the basal space calculated by Bragg's equations 49 at 12.04 nm. Another prominent peak is at the 28.5°, the peak of the (003) surface of montmorillonite, as reported by Orucoglu et al 50 As also seen in the preattritor Na-MMT curve (Figure 5g), along with prominent montmorillonite peaks, Illite was found at around 8.8°, clinoptilolite at 10.2°, and quartz, calcite, and dolomite minerals at 27, 28.5, and 29.5°, respectively. Similar findings were obtained from the same samples previously studied by Bulut et al, Orucoglu et al, and O ̈nal et al 48,50,51 However, it is quite difficult to make these inferences from the XRD pattern of postattritor nano-MMT.…”
Section: Ee%supporting
confidence: 82%
“…Modification of natural bentonite with a surfactant is an easy method to change the nature of the bentonite surface hydrophilic to hydrophobic [9][10][11]. The negative charge on the surface of the silica layer of bentonite can be attached to the polar compounds and cations in the interlayer of bentonite can be exchanged with organic cations [11][12][13][14]. The structure and texture of nature and organically modified montmorillonite were characterized using various methods, such as XRD, FT-IR, SEM-EDX-mapping and surface area measurements along with the chemical analysis.…”
Section: Introductionmentioning
confidence: 99%
“…Bentonite, among various clay minerals, emerges as a naturally abundant material endowed with the potential for enhanced adsorption capacity through the insertion of organic moieties into its interlaminar spaces [15][16][17]. Nevertheless, the inherent hydrophilicity of raw bentonite restricts its efficacy in adsorbing organic pollutants, including phenols [18]. To surmount this limitation, surfactant modification has arisen as a promising strategy to enhance the adsorption efficiency of bentonite by modifying its surface chemistry and ameliorating its porous structure [9,18,19].…”
Section: Introductionmentioning
confidence: 99%
“…Nevertheless, the inherent hydrophilicity of raw bentonite restricts its efficacy in adsorbing organic pollutants, including phenols [18]. To surmount this limitation, surfactant modification has arisen as a promising strategy to enhance the adsorption efficiency of bentonite by modifying its surface chemistry and ameliorating its porous structure [9,18,19]. By introducing organic compounds, the resultant organo-bentonite exhibits enhanced pollutant removal capacities in aquatic environments [18,20,21].…”
Section: Introductionmentioning
confidence: 99%