Abstract
Opalinus clay has a high sealing capacity and is therefore considered as a viable candidate for hosting high-level radioactive waste. Assessment of long-term containment function of clays requires understanding and modelling mass transport through evolving pore systems. Development of pore network models for diffusion, which can be coupled to models for deformation and micro-cracking, is reported. Effects of clay texture and solid phase constitution are calculated and analysed. The results are in the range of, but slightly over-predicting, experimentally measured coefficients of diffusion in different clay directions. Further model improvements require better knowledge of micro-pore turtuosity, which awaits higher resolution experimental techniques.
| Original language | English |
|---|---|
| Pages (from-to) | 1369-1377 |
| Number of pages | 8 |
| Journal | Mineralogical Magazine |
| Volume | 79 |
| Issue number | 6 |
| DOIs | |
| Publication status | Published - 1 Dec 2015 |
Keywords
- Clays
- Radioactive waste
- Mass transport
- Microstructure
- Pore networks