2009
DOI: 10.1016/j.clay.2009.07.007
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Charge location effect on the hydration properties of synthetic saponite and hectorite saturated by Na+, Ca2+ cations: XRD investigation

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Cited by 30 publications
(32 citation statements)
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“…Also, an increase in the saponite layer charge enhances the interlayer hydration . Karmous et al (2009) conducted hydration experiments at standard pressure and temperature by forcing the relative humidity (90 %) on saponites similar to those considered (i.e., the same layer charge). His results indicate the incorporation of two layers of water, leading to a potential maximal expansion of the basal spacing at 16.32 Å when Ca is in the interlayer sheet, and 14.99 Å when Na is in the interlayer sheet.…”
Section: Geochemical Model Setupmentioning
confidence: 99%
“…Also, an increase in the saponite layer charge enhances the interlayer hydration . Karmous et al (2009) conducted hydration experiments at standard pressure and temperature by forcing the relative humidity (90 %) on saponites similar to those considered (i.e., the same layer charge). His results indicate the incorporation of two layers of water, leading to a potential maximal expansion of the basal spacing at 16.32 Å when Ca is in the interlayer sheet, and 14.99 Å when Na is in the interlayer sheet.…”
Section: Geochemical Model Setupmentioning
confidence: 99%
“…X-ray diffraction (XRD) experiments have been applied for investigating the interlayer cation states via a variation of the basal spacing upon hydration. [10][11][12] The uniform distribution of interlayer cations without any specific structure has been implied in the previous studies. In the present study, the interlayer cation states, which can be varied via the local structure of the 2D nanosheets, were highlighted based on the data of solid-state 23 Na nuclear magnetic resonance (NMR) spectroscopy.…”
mentioning
confidence: 67%
“…These negative charges in MMT surface come from the isomorphic substitution that is the replacement of Al 3+ by other divalent cations like Mg 2+ and Fe 2+ in the octahedral sheet or the replacement of Si 4+ by Al 3+ in the tetrahedral sheet of the MMT layer. Previous works28–30 demonstrated that surface charge density of clay layers and charge locations were crucial to the swelling and flocculation of the clay platelets and the clay/water interactions. Currently, we believe it is quite possible that for the natural MMT minerals, due to the wide distribution of the local surface charge density, not all MMT platelets exfoliated into monolayers when dispersed in water; some stacked structure with very less MMT layers might still be there in the aqueous suspension, which is hard to be tested by instruments.…”
Section: Resultsmentioning
confidence: 98%