Abstract
Bentonite consists of nanometer scale of smectitic clay minerals (mainly montmorillonite) and micrometer scale of macro-grains (mainly quatz). Properties of saturated bentonite are characterized by hydrated clay minerals. For a diffusion problem in bentonite we developed a new multiscale homogenization analysis (HA) procedure which relates microscale characteristics with a macroscopic behavior. We discuss diffusion properties of tritium water (HTO) compared with experimental data. Microscopic properties of the montmorillonite hydrate such as diffusivity of chemical species which are used in HA are determined by a molecular dynamics (MD) simulation method. We show the calculated results are consistent with macroscale experimental data.
| Original language | English |
|---|---|
| Pages (from-to) | 117-124 |
| Number of pages | 8 |
| Journal | Materials Science Research International |
| Volume | 9 |
| Issue number | 2 |
| Publication status | Published - Jun 1 2003 |
Keywords
- Bentonite
- Diffusion
- Geological disposal
- HTO
- Molecular dynamics
- Montmorillonite hydrate
- Multiscale homogenization analysis
ASJC Scopus subject areas
- Materials Science(all)
Fingerprint Dive into the research topics of 'Micro-structure of bentonite clay and diffusion coefficient given by multiscale homogenization analysis'. Together they form a unique fingerprint.
Cite this
Fujii, N., Ichikawa, Y., Kawamura, K., Suzuki, S., & Kitayama, K. (2003). Micro-structure of bentonite clay and diffusion coefficient given by multiscale homogenization analysis. Materials Science Research International, 9(2), 117-124.