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Self-assembly Processes in Hydrated Montmorillonite by FTIR Investigations
Maria Teresa Caccamo1, Giuseppe Mavilia1, Letterio Mavilia2
1Dipartimento di Scienze Matematiche e Informatiche, Scienze Fisiche e Scienze della Terra, Università di Messina, Viale Ferdinando Stagno D'Alcontres n 31, S. Agata, 98166 Messina, Italy.
Materials (Basel, Switzerland)
|March 4, 2020
Summary
Fourier-transform infrared (FTIR) and Raman spectroscopy reveal how water behaves in montmorillonite clay. Ordered water leaves faster than disordered water during dehydration, promoting clay layer self-assembly.
Area of Science:
- Materials Science
- Spectroscopy
- Clay Science
Background:
- Montmorillonite clay's interaction with water is crucial for its properties.
- Understanding the hydrogen bond network of water within clay structures is complex.
Purpose of the Study:
- To investigate the time-dependent behavior of water within montmorillonite.
- To analyze the hydrogen bond network of water during clay dehydration.
Main Methods:
- Utilized Fourier-transform infrared (FTIR) and Raman spectroscopies.
- Analyzed OH stretching modes using Gaussian components and wavelet cross-correlation.
- Monitored samples over time at various montmorillonite-water concentrations.
Main Results:
- Total water content in montmorillonite decreases over time.
- Ordered water diminishes faster than disordered water during dehydration.
- Residual disordered water remains entrapped in the clay structure longer.
Conclusions:
- Dehydration of montmorillonite leads to changes in water structure.
- The differential release of ordered and disordered water influences clay behavior.
- Montmorillonite dehydration promotes layer self-assembly.
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