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Surface Instability of Serpentine in Aqueous Suspensions
Tartaj1, Cerpa, García-González
1Instituto de Ciencia de Materiales de Madrid (CSIC), Campus de Cantoblanco, Madrid, 28049, Spain
Journal of Colloid and Interface Science
|November 18, 2000
Summary
The surface charge of lizardite serpentines in water depends on their alteration grade. Alteration affects the magnesium-to-silicon ratio, influencing electrokinetic behavior and suspension stability.
Area of Science:
- Mineralogy
- Surface Chemistry
- Colloid Science
Background:
- Serpentine minerals, specifically lizardite, are common in various geological settings.
- Understanding the electrokinetic behavior of mineral suspensions is crucial for applications in mining, environmental remediation, and materials science.
Purpose of the Study:
- To investigate the electrokinetic behavior and stability of aqueous suspensions of lizardite serpentines.
- To correlate surface properties with mineral composition and alteration grade.
Main Methods:
- Crystallochemical analyses: X-ray diffraction, IR spectroscopy, Transmission Electron Microscopy (TEM), Differential Thermal Analysis/Thermogravimetric Analysis (DTA/TG), X-ray Fluorescence (XRF).
- Electrokinetic measurements to determine surface charge and isoelectric point.
- Dissolution studies to assess mineral alteration.
Main Results:
- All studied samples were identified as lizardite-type serpentines with similar chemical compositions.
- Electrokinetic behavior is primarily governed by the surface Mg/Si atomic ratio.
- Lower isoelectric points correlate with Mg/Si ratios below the ideal lizardite value (1.5).
- Incongruent dissolution leads to surface enrichment of silicon.
Conclusions:
- The surface charge of lizardite in aqueous interfaces is directly dependent on the degree of surface alteration.
- Mineral alteration significantly impacts the electrokinetic properties and stability of serpentine suspensions.
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