2009
DOI: 10.1021/cm902800y
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Facile Scalable Synthesis of Rectorites

Abstract: Using a synthetic Na-fluorohectorite ([Na 0.5 ] inter [Mg 2.5 Li 0.5 ] oct [Si 4 ] tet O 10 F 2 ), mixed-cation heterostructures with an alternating interstratification pattern are formed under appropriate conditions via simple cation-exchange reactions. The most important requirement for the spontaneous formation of these ordered mixed-layer structures is a high degree of charge homogeneity of the smectite. The partial exchange of cations with largely different hydration enthalpies (Na þ by K þ ) results in t… Show more

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Cited by 36 publications
(49 citation statements)
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“…Several experimental studies showed the hydration and dehydration properties of rectorite with different cations. 38, 39 With the rapid development of rectorite-based composites, industrial applications of rectorite are increasing. 40−44 The complicated structure of rectorite makes it more difficult to obtain exact interlayer information by experiments than that of montmorillonite.…”
Section: ■ Introductionmentioning
confidence: 99%
“…Several experimental studies showed the hydration and dehydration properties of rectorite with different cations. 38, 39 With the rapid development of rectorite-based composites, industrial applications of rectorite are increasing. 40−44 The complicated structure of rectorite makes it more difficult to obtain exact interlayer information by experiments than that of montmorillonite.…”
Section: ■ Introductionmentioning
confidence: 99%
“…larger platelets, less impurities and higher homogeneities. [20][21][22] Moreover, designed synthesis allows to adjust crucial parameters controlling accessible aspect ratios: nature of interlayer cation, layer charge, and composition. Colorless materials can easily be produced and the intracrystalline reactivity may be adjusted to a level where switching between shear stiff and shear labile states allows to alter the effi ciency of tactoid exfoliation.…”
mentioning
confidence: 99%
“…In literature, the narrow 23 Na peak at ca. 0 ppm is attributed to trapped Na + ions in symmetric cavities created by a mica-type stacking or to nonexchangeable part of the sodium interlayer cations (Möller et al, 2010). In contrast to that work, the quadrupolar interactions for this peak are not averaged out, and it can tentatively be assigned to a variety of Na-containing mica in the samples under study.…”
Section: Nmrmentioning
confidence: 60%