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Open AccessJournal ArticleDOI

Intercalation of sugar alcohols into the interlayer of montmorillonite by wet and dry processes

TLDR
In this article, the authors showed that the d-spaces of the resulting complexes formed by the wet intercalation process were about 0.4 nm larger than those formed by a dry intercation process.
Abstract
Organic and inorganic complexes are formed by the intercalation of ethylene glycol and glycerol into the interlayer of montmorillonite. Glycerol and ethylene glycol have the molecular formula C 2 H 6 O 2 and C 3 H 8 O 3 , respectively, and the general formula is C n H 2(n+1) O n . This formula represents a sugar alcohol group: erythritol for n = 4, xylitol for n = 5, sorbitol for n = 6, and so on. Complexes were produced by a wet process, in which erythritol, xylitol and sorbitol solutions, and montmorillonite, were mixed to a paste; and by a dry process, in which montmorillonite and erythritol, xylitol and sorbitol, in the solid state, were mixed by automatic agate mortar. X-ray diffraction, FT-IR and X-ray photoelectron spectroscopy analyses of the resulting complexes showed that erythritol, xylitol and sorbitol were intercalated into the interlayer of montmorillonite in both wet and dry processes. The resulting complexes also showed an increase in the basal spacing with increasing n (or molecular weight or carbon chains). The difference between the wet and dry processes lies in the d-spacing in each montmorillonite-sugar alcohol system. The d-spacing of the complexes formed by the wet intercalation process were about 0.4 nm larger than those formed by the dry intercalation process. This is the length of the longest part of the water molecule. In the wet process, the sugar alcohols were intercalated with water molecules, and the montmorillonite swelled, while it expanded in the dry process.

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Variation of preserving organic matter bound in interlayer of montmorillonite induced by microbial metabolic process.

TL;DR: The results showed that the montmorillonite under the influence of soil bacteria has a strong buffering capacity for preserving organic matter into the interlayer space in a short-term.
References
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Journal ArticleDOI

Correlation of O-H Stretching Frequencies and O-H O Hydrogen Bond Lengths in Minerals

TL;DR: In this article, a correlation of O-H stretching frequencies (from infrared spectroscopy) with O…O and H…O bond lengths (from structural data) of minerals was established.
Journal ArticleDOI

Ethylene glycol and glycerol complexes of smectites and vermiculites

TL;DR: In this article, the authors proposed a method for the detection of organo-silicate complexes formed by ethylene glycol, HOCH2.CH2OH, and glycerol HOCH 2.CHOH.
Journal ArticleDOI

Identification of the Montmorillonite Group of Minerals by X-Rays

TL;DR: This group of clay minerals, referred to hereafter for brevity simply as "montmorillonite", is characterized by the variation of the position of the basal reflexion on an X-ray powder or aggregate diagram, from about 10 to about 18 A, according to the state of hydration.
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