Images
XFEM - an illustration of a XFEM enrichment in 2d
- 2 aquifer system communicating through 5 wells
- 2d singular enrichment of pressure
- the underlying coarse mesh is at the bottom
XFEM - an illustration of a XFEM enrichment in 3d
- 3d bulk rock is cut by 10 wells
- 1d-3d singular enrichment of velocity
DGR_1 - Deep geological repository model
- model of DGR for future spent nuclear fuel
- fractured granit massive of approximately 500m scale
- piezometric head is displayed, including the subsurface view
DGR_2 - Deep geological repository 3d model
- model of DGR for future spent nuclear fuel
- fractured granit massive of approximately 200 km2
- left - computational mesh, including main faults
- right - piezometric head is displayed at the level of DGR (-500m)
Bedřichov - model of granit massive in the Jizera mountains
- transport of natural tracers is modeled and compared extensive data collection measured on site
- extensive measurements are collected online in the underground tunnel
- piezometric head and velocity are displayed
- detail of the tunnel cut by fractures is presented at the bottom
DFN - Discrete fracture network 2d demonstration
- comparison of rock properties with different fracture network around tunnel excavation
- left - homogenous rock
- middle - stochastic DFN generated
- right - stochastic DFN and some major deterministic faults
- pressure is displayed, zero Dirichlet BC considered for simplification
Videos
Transport - an illustration of concentration propagation through fractured rock
- 2d model of fractured porous media
- advection-diffusion equation solved on 1d-2d compatible mesh
- concentration propagates through the fractures faster than through the bulk rock
Transport solver - comparison of different methods
- 1d problem with moving concentration peak
- Finite volumes - piecewise constant solution, large numerical diffusion can be observed
- Finite elements - piecewise linear solution, some oscillations are present
- Discontinuous Galerkin - piecewise linear solution, no oscillations and minimal diffusion