2019
DOI: 10.1007/s42860-019-00046-9
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Giant Multistep Crystalline vs. Osmotic Swelling of Synthetic Hectorite in Aqueous Acetonitrile

Abstract: Intercalation of large organocations into 2:1 clay minerals may be hampered by two problems: on one hand, the solubility of organocations in water is limited and the resulting high selectivity for adsorption in the polar solvent may lead to non-equilibrium structures. On the other hand, the large expansion of the interlayer space will slow down kinetics of ion exchange considerably. The best workaround for these obstacles is to suspend the clay minerals in mixtures of water with more hydrophobic organic solven… Show more

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Cited by 14 publications
(20 citation statements)
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“…The crystalline and osmotic swelling are commonly found in clay minerals. 157,[212][213][214][215] Remarkably, crystalline swelling is found for Brodie GO in all so far studied solvents except for water, while for Hummers GO only osmotic swelling has so far been reported. Crystalline swelling provides an opportunity to evaluate the thickness of solvent layers confined between GO sheets.…”
Section: Swelling Of Graphite Oxide In Solvents Other Than Watermentioning
confidence: 96%
“…The crystalline and osmotic swelling are commonly found in clay minerals. 157,[212][213][214][215] Remarkably, crystalline swelling is found for Brodie GO in all so far studied solvents except for water, while for Hummers GO only osmotic swelling has so far been reported. Crystalline swelling provides an opportunity to evaluate the thickness of solvent layers confined between GO sheets.…”
Section: Swelling Of Graphite Oxide In Solvents Other Than Watermentioning
confidence: 96%
“…For fast kinetics of the intercalation of [Cu(dppb) 2 ] + the one‐layer hydrate of Na + ‐hec was first swollen in acetonitrile: water mixture (75:25 vol%) (Figure 1a). Swelling in this solvent mixture is limited to the crystalline regime and the basal spacing [ 17 ] expanded in this mixture from d 001 = 12.3 Å for the one‐layer hydrate [ 11 ] to 30.7 Å for the crystalline swollen Na + ‐hec (Figure S1b, Supporting Information), as determined by means of small‐angle X‐ray scattering (SAXS). Enlarging the gap opening between adjacent silicate layers to ≈21 Å (subtracting the layer thickness of hectorite, 10 from 30.7 Å) facilitates the intercalation of the bulky metal‐complex ions [Cu(dppb) 2 ] + of ≈10 Å.…”
Section: Resultsmentioning
confidence: 99%
“…Only the latter are capably to swell osmotically. [ 9c,17 ] When immersing the alternating heterostructure into deionized, pure water, the crystal forceless and spontaneously delaminates into double‐stacks, where a hydrophobic monolayer of [Cu(dppb) 2 ] + is encapsulated between the two thin silicate layers (Figure 1c).…”
Section: Resultsmentioning
confidence: 99%
“…Osmotic swelling is controlled by the relatively easy flow of solvent in and out of structure regulated by osmotic effects. [29][30][31][32][33] Remarkably, crystalline swelling is found for Brodie GO in all so far studied solvents except water [34][35][36][37][38] while for Hummers GO only osmotic-like swelling was so far reported. [37,39,40] Adding water to clays under conditions of confinement is known to produce pressures in the range of tens or even hundreds of bar.…”
mentioning
confidence: 93%
“…Osmotic swelling is controlled by the relatively easy flow of solvent in and out of structure regulated by osmotic effects. [ 29–33 ] Remarkably, crystalline swelling is found for Brodie GO in all so far studied solvents except water [ 34–38 ] while for Hummers GO only osmotic‐like swelling was so far reported. [ 37,39,40 ]…”
Section: Introductionmentioning
confidence: 99%