1996
DOI: 10.1180/claymin.1996.031.3.04
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Effect of non-swelling layers on the dissolution of reduced-charge montmorillonite in hydrochloric acid

Abstract: A series of reduced-charge montmorillonites (RCM), prepared from the same parent Li-montmorillonite (Jelgov2? Potok, Slovakia) by heating at various temperatures (105-210~ for 24 h, was treated with 6 M HC1 at 95~ for periods up to 30 h. Reaction solutions obtained were analysed for A1, Fe, Mg and Li and the solid reaction products were investigated by FrlR spectroscopy. Both analyses provided evidence that the extent of dissolution decreased with increased amounts of Li fixed within the montmorillonite struct… Show more

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Cited by 92 publications
(48 citation statements)
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“…The characteristic band at 915 cm À1 is due to Al À Al À OH stretching in the octahedral layer and the band at 538 cm À1 is due to the Al À O À Si stretching mode. [25,26] For APZ-MMT and AEAcoated APZ-MMT, the characteristic bands of APZ were overlapped in their spectra (Figure 2 A, spectra c and d), thus indicating that the APZ molecules were stabilized in the interlayer space through electrostatic interactions without structural changes. However, after hybridization, the OH stretching peak, which was observed at 3443 cm À1 with pristine MMT, shifted to a lower wavenumber (3428 cm À1 ), owing to the interactions between APZ and MMT, which proceeded through a water-bridging mechanism (Figure 2 B).…”
Section: Resultsmentioning
confidence: 92%
“…The characteristic band at 915 cm À1 is due to Al À Al À OH stretching in the octahedral layer and the band at 538 cm À1 is due to the Al À O À Si stretching mode. [25,26] For APZ-MMT and AEAcoated APZ-MMT, the characteristic bands of APZ were overlapped in their spectra (Figure 2 A, spectra c and d), thus indicating that the APZ molecules were stabilized in the interlayer space through electrostatic interactions without structural changes. However, after hybridization, the OH stretching peak, which was observed at 3443 cm À1 with pristine MMT, shifted to a lower wavenumber (3428 cm À1 ), owing to the interactions between APZ and MMT, which proceeded through a water-bridging mechanism (Figure 2 B).…”
Section: Resultsmentioning
confidence: 92%
“…Collapsed, pyrophyllite-like layers are formed upon nearly complete charge reduction (85-90%) in Li-saturated dioctahedral smectites with an initial layer charge located in the octahedral sheets (Brindley and Ertem, 1971;Ertem, 1972;Lim and Jackson, 1986;BujdSk et al, 1991BujdSk et al, , 1992Komadel et al, 1996). This transformation has been used to distinguish montmorillonite from beidellite (Greene-Kelly, 1953;Schultz, 1969;Lim and Jackson, 1986).…”
Section: Layer Charge Reductionmentioning
confidence: 99%
“…Johnston et al (1992) and Schuttlefield et al (2007) used FTIR to study water interactions and uptake, respectively, onto clay minerals. Komadel et al (1996) monitored HCl and temperature-induced structural changes in reduced-charge montmorillonites via FTIR analyses. Octahedral sheet evolution with progressive kaolinization was studied by Cuadros and Dudek (2006) using mixed kaolinite-smectite samples and transmission FTIR spectroscopy.…”
Section: Phyllosilicatesmentioning
confidence: 99%