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Published on: September 5, 2019
A multiscale approach to ion diffusion in clays: building a two-state diffusion-reaction scheme from microscopic
Benjamin Rotenberg1, Virginie Marry, Jean-François Dufrêche
1Université Pierre et Marie Curie-Paris 6, Laboratoire Liquides Ioniques et Interfaces Chargées, UMR CNRS 7612, 4 pl. Jussieu, Paris cedex F-75005, France. rotenber@ccr.jussieu.fr
Particle mobility in confining media, like charged clays, is reduced by surface interactions. This study models ion dynamics, revealing how surface interactions control mobility and ion distribution coefficients (Kd).
Area of Science:
- Colloid and Surface Science
- Computational Chemistry
- Environmental Science
Background:
- Particle mobility is reduced in confining media due to geometry and surface interactions.
- The water/mineral interface critically influences ion dynamics in materials like clays.
- Ionic mobility in clays involves diffusion and surface trapping.
Purpose of the Study:
- To develop a two-state diffusion-reaction scheme for ion dynamics.
- To model ion interactions with mineral surfaces.
- To determine ion mobility within clay interlayers.
Main Methods:
- Molecular simulations for atomic-level ion dynamics in clay interlayers.
- Development of a mesoscopic Fokker-Planck model from simulation data.
- Derivation of a diffusion-reaction scheme and distribution coefficient (Kd).
Main Results:
- Microscopic dynamics were captured using molecular simulations.
- A robust mesoscopic Fokker-Planck description was established.
- Ion mobility and the distribution coefficient (Kd) were determined.
Conclusions:
- A multi-scale modeling approach links atomic dynamics to macroscopic ion mobility.
- The distribution coefficient (Kd) is crucial for understanding electrokinetic phenomena in porous materials.
- This framework provides insights into ion transport influenced by mineral surface interactions.
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