2002
DOI: 10.1006/jcis.2002.8654
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Influence of the Layer Charge and Clay Particle Size on the Interactions between the Cationic Dye Methylene Blue and Clays in an Aqueous Suspension

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Cited by 126 publications
(81 citation statements)
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“…In contrast to similar investigations on MB/clay composites, [43,46] the structures on GO do not change with adsorption time. It can be concluded that the interaction of MB with the reactive oxygen groups of the GO surface is stronger than that with the surface hydroxyl groups of clays.…”
contrasting
confidence: 81%
See 1 more Smart Citation
“…In contrast to similar investigations on MB/clay composites, [43,46] the structures on GO do not change with adsorption time. It can be concluded that the interaction of MB with the reactive oxygen groups of the GO surface is stronger than that with the surface hydroxyl groups of clays.…”
contrasting
confidence: 81%
“…[43,44] Clays with their layered structures allow a wide range of MB aggregation, including intercalation, [45] cation exchange, [46] and fluorescence labeling. [47] Graphite oxide exhibits a similar layered structure and anionic surface charges to clays.…”
Section: Introductionmentioning
confidence: 99%
“…The characteristic differences between the electronic absorption spectra of monomers, dimers, and higher aggregates have been used to distinguish them. [3][4][5][6][7][8] MB interacts with different materials such as colloids, [8][9][10][11][12] metallic surfaces, [13] silica, [14][15][16] nano-objects, [17,18] polymers, [19] cyclodextrins, [20][21][22] and form complexes with other low-molecular-weight molecules. [22][23][24] Its state of aggregation may change as a consequence of these interactions.…”
Section: Introductionmentioning
confidence: 99%
“…If the surface charge density is high, then the clay mineral is non-swellable, and, of course, the cations are not exchangeable [22,23]. Consequently, the CEC is small, because only the outer surface is available.…”
Section: Selection Of the Clay Mineralsmentioning
confidence: 99%