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Interlayer structural and confined water effects in kaolinite–alcohol systems via dimethyl sulfoxide intercalation

Published online by Cambridge University Press:  14 September 2026

Ding Wang
Affiliation:
Hebei GEO University, China
Jiawei Li
Affiliation:
Hebei GEO University, China
Wenxu Liu
Affiliation:
Hebei GEO University, China
Changjiang Liu
Affiliation:
Hebei GEO University, China
Chuncheng Yang
Affiliation:
Hebei GEO University, China
Yan Li*
Affiliation:
Hebei GEO University, China
*
Corresponding author: Yan Li; Email: liyan1@hgu.edu.cn
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Abstract

Methanol- and ethylene glycol-grafted kaolinite were prepared via a stepwise intercalation–grafting strategy using dimethyl sulfoxide-intercalated kaolinite as an intermediate, with the aim of elucidating the structural differences between the two grafted products and clarifying the role of interlayer water. The products were systematically characterized by X-ray diffraction (XRD), Fourier-transform infrared (FTIR) spectroscopy, solid-state magic-angle spinning nuclear magnetic resonance (MAS NMR), elemental analysis (CHNS) and thermogravimetry–differential scanning calorimetry (TG–DSC). Compared with methoxy-modified kaolinite, the ethylene glycol-grafted kaolinite exhibited enhanced structural ordering, greater organic loading and improved thermal stability. The covalently grafted ethylene glycol molecules adopt a trans configuration in the interlayers of kaolinite, accompanied by a minute fraction of non-bonded ethylene glycol molecules and some amount of interlayer water molecules. Although the confined water in both systems originated from condensation reaction, it probably played opposite roles: it facilitated the ethylene glycol grafting while hindering that for methanol.

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Article
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© The Author(s), 2026. Published by Cambridge University Press on behalf of The Mineralogical Society of the United Kingdom and Ireland.
Figure 0

Table 1. The chemical composition by percentage mass of the original kaolinite.Table 1 long description.

Figure 1

Figure 1. XRD traces of kaolinite, Kaol-DMSO, Kaol-MeOH and Kaol-EG: (a) full-range XRD traces and (b) enlarged (001) region.Table 1 long description.

Figure 2

Figure 2. FTIR spectra of kaolinite, Kaol-DMSO, Kaol-MeOH and Kaol-EG in the regions of (a) 3800–2800 cm–1 and (b) 1800–800 cm–1.Figure 2 long description.

Figure 3

Figure 3. (a) 13C MAS NMR spectra of Kaol-DMSO, Kaol-MeOH and Kaol-EG and (b) 1H MAS NMR spectrum of Kaol-EG.

Figure 4

Table 2. Elemental contents (carbon, hydrogen, sulfur) of Kaol-DMSO, Kaol-MeOH and Kaol-EG and the calculated chemical formulas.Table 2 long description.

Figure 5

Figure 4. (a) TG and (b) DSC curves of kaolinite, Kaol-DMSO, Kaol-MeOH and Kaol-EG.Figure 4 long description.

Figure 6

Figure 5. Schematic representation of the transformation from kaolinite to Kaol-DMSO, Kaol-MeOH and Kaol-EG. Al = dark grey; C = black; H = white; O = red; Si = yellow.Figure 5 long description.

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