| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | Comparison of alternative approaches to modelling gas migration through a higher strength rock |
|---|
| Journal | Mineralogical Magazine |
|---|
| Authors | Hoch, A. R. | Author |
|---|
| James, M. | Author |
| Year | 2012 (December) | Volume | 76 |
|---|
| Issue | 8 |
|---|
| Publisher | Mineralogical Society |
|---|
| DOI | doi:10.1180/minmag.2012.076.8.44Search in ResearchGate |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 244347 | Long-form Identifier | mindat:1:5:244347:2 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | Hoch, A. R., James, M. (2012) Comparison of alternative approaches to modelling gas migration through a higher strength rock. Mineralogical Magazine, 76 (8) 3319-3326 doi:10.1180/minmag.2012.076.8.44 |
|---|
| Plain Text | Hoch, A. R., James, M. (2012) Comparison of alternative approaches to modelling gas migration through a higher strength rock. Mineralogical Magazine, 76 (8) 3319-3326 doi:10.1180/minmag.2012.076.8.44 |
|---|
| Abstract/Notes | AbstractThe Radioactive Waste Management Directorate of the UK Nuclear Decommissioning Authority has prepared a generic disposal system safety case (DSSC) that covers a range of possible host rock environments. In many of the waste packages considered in the DSSC, the formation of gases by chemical and microbial processes is likely to occur. In order to demonstrate safety, it is necessary to understand the rates at which the gases are generated and their subsequent migration from a disposal facility after closure. This paper is concerned with modelling gas migration through a fractured higher strength host rock. A first set of simulations compares alternative approaches to modelling gas migration through a fractured rock. The approaches differ in their representation of the interaction between the fractures and the rock matrix. As expected, the gross features of many of the simulations are very similar, with a single continuum approach in which the porosity is set equal to either the fracture porosity or the matrix porosity providing the bounding cases. Gas migration is slower for those simulations where the gas can access more of the rock matrix. A final simulation, with a heterogeneous permeability field, is compared with the other simulations, again showing a very similar evolution. |
|---|
These are possibly similar items as determined by title/reference text matching only.
