Differences
This shows you the differences between two versions of the page.
Both sides previous revision Previous revision Next revision | Previous revision Last revision Both sides next revision | ||
test_cases:five [2014/10/24 14:26] grenier |
test_cases:five [2020/06/30 16:15] grenier |
||
---|---|---|---|
Line 1: | Line 1: | ||
**Case TH2: the initial frozen inclusion** | **Case TH2: the initial frozen inclusion** | ||
- | This is the first benchmark case with the full system of equations: | + | This is the first benchmark case with the full system of equations. |
- | + | ||
- | {{ equations.jpg?300 }} | + | |
Initial conditions correspond to a fully saturated porous medium with a frozen inclusion (-5°C) within a temperate surrounding (5°C): | Initial conditions correspond to a fully saturated porous medium with a frozen inclusion (-5°C) within a temperate surrounding (5°C): | ||
- | + | {{ : | |
- | {{ cas1.jpg?300 }} | + | |
Boundary conditions are for the left boundary imposed positive temperature (5°C) and zero temperature gradient for the other limits (zero heat conductive fluxes). Water transfer boundary conditions are uniform flow from left (inflow) to right (outflow) as sketched below | Boundary conditions are for the left boundary imposed positive temperature (5°C) and zero temperature gradient for the other limits (zero heat conductive fluxes). Water transfer boundary conditions are uniform flow from left (inflow) to right (outflow) as sketched below | ||
Line 19: | Line 16: | ||
- | // | + | **The whole information related with Benchmark Case TH2 (including parameter |
+ | |||
+ | **The results are now published and available from the [[intercomparaison_results: | ||
- | ... |