| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | Thermal cycling: impact on bentonite permeability |
|---|
| Journal | Mineralogical Magazine |
|---|
| Authors | Zihms, S. G. | Author |
|---|
| Harrington, J. F. | Author |
| Year | 2015 (November) | Volume | 79 |
|---|
| Issue | 6 |
|---|
| Publisher | Mineralogical Society |
|---|
| DOI | doi:10.1180/minmag.2015.079.6.29Search in ResearchGate |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 244728 | Long-form Identifier | mindat:1:5:244728:9 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | Zihms, S. G., Harrington, J. F. (2015) Thermal cycling: impact on bentonite permeability. Mineralogical Magazine, 79 (6) 1543-1550 doi:10.1180/minmag.2015.079.6.29 |
|---|
| Plain Text | Zihms, S. G., Harrington, J. F. (2015) Thermal cycling: impact on bentonite permeability. Mineralogical Magazine, 79 (6) 1543-1550 doi:10.1180/minmag.2015.079.6.29 |
|---|
| Abstract/Notes | AbstractDue to its favourable properties, in particular, low permeability and swelling capacity, bentonite has been favoured as an engineered-barrier and backfill material for the geological storage of radioactive waste. To ensure its safe long-term performance it is important to understand any changes in these properties when the material is subject to heat-emitting waste. As such, this study investigates the hydraulic response of bentonite under multi-step thermal loading subject to a constant-volume boundary condition, to represent a barrier system used in a crystalline or other hard-rock host rock. The experimental set up allows continuous measurement of the hydraulic and mechanical responses during each phase of the thermal cycle. After the initial hydration of the bentonite, the temperature was raised in 20°C increments from 20 to 80°C followed by a final step to reach 120°C. Each temperature was held constant for at least 7–10 days to allow the hydraulic transients to equilibrate. The data suggest that the permeability of bentonite appears to be sensitive to changes in temperature which may extend beyond those explained by simple changes in water viscosity. However, permeability may be boundary-condition dependent and this should be considered when designing experiments or applying these results to other repository host rocks. Either way, the magnitude of the change in permeability observed in this study is minor and its impact on the hydraulic performance of the barrier is negligible. |
|---|
These are possibly similar items as determined by title/reference text matching only.
