A verified numerical simulator for hydro-geomechanical heterogeneity based on MOOSE
RHEA (Real HEterogeneity App), is an open-source fully coupled finite element application capable of including element-resolution hydro-geomechanical properties in coupled simulations. The code was developed by José Bastías with small additions from Andy Wilkins in a collaboration between Karlsruhe Institute of Technology (KIT) and the Commonwealth Scientific and Industrial Research Organisatio (CSIRO).
RHEA is a MOOSE based application, for more information visit MOOSE Framework. To use RHEA, you will need to have installed MOOSE, which can take some time.
RHEA is released under the GNU Lesser General Public License Version 2.1. See the LICENSE file for details.
For system requirements and MOOSE installation visit Getting Started page of the MOOSE framework.
The stable version of RHEA can be cloned directly for the GitHub repository. As usual in any MOOSE based app, RHEA will be located by default in the cd ~/projects
foulder generated during the installation of MOOSE.
cd ~/projects
git clone https://github.com/josebastiase/RHEA.git
cd ~/projects/RHEA
git checkout master
As any MOOSE based app, you first need to compile RHEA
cd ~/projects/RHEA
make -j4
and then test RHEA
cd ~/projects/RHEA
./run_tests
If RHEA has compiled successfully, you should see various output, ending with the line
2 passed, 0 skipped, 0 pending, 0 failed
In Terzaghi’s original theoretical work (von Terzaghi, 1923), which was inspired by the measurements of delayed deformations in a compression test on a clay sample, the pore fluid and the soil particles were both assumed to be incompressible, so that the only mechanism of deformation was a rearrangement of the particles. In modern presentations, these assumptions are no longer made, and this generalised theory will be used here. The relevant parameters used in this model are as follows.
Hydraulic properties
Parameter | Symbol | Value | Unit |
---|---|---|---|
Hydraulic conductivity | k | 1.0E-4 | m/s |
Porosity | n | 0.2 | - |
Mechanical properties
Parameter | Symbol | Value | Unit |
---|---|---|---|
Shear modulus | G | 6.25E7 | Pa |
Bulk modulus | K | 8.4E7 | Pa |
Biot's coefficient | a | 0.9 | - |
Fluid properties
Parameter | Symbol | Value | Unit |
---|---|---|---|
Water bulk modulus | K_f | 2.2E7 | Pa |
Volumetric weigth | y | 1.0E4 | m/s |
System's characteristics
Parameter | Symbol | Value | Unit |
---|---|---|---|
Load | q | 1.0E3 | Pa |
System's depth | h | 1.0E2 | m |
time | t | - | s |
The RHEA files for this scenario are found in test/tests/terzaghi/
. There are three important files:
-
test/tests/terzaghi/Workflow_TerzaghiImportData.ipynb
. This is a Jupyter notebook that creates files that define the hydraulic conductivity, porosity, bulk modulus and shear modulus throughout the Terzaghi soil sample. In this case, these properties are homogeneous. The files created areK.data
,p.data
,L.data
andG.data
(which are part of this repository, so you don't need to create them yourself). -
test/tests/terzaghi/TerzaghiImportData.i
. This is the RHEA input file. Run it using therhea-opt
executable you created during compilation:../../../rhea-opt -i TerzaghiImportData.i
. -
test/tests/terzaghi/plot_results.py
. This is a python file that plots the results, demonstrating agreement between RHEA and the analytical formulae derived by Terzaghi:
The Terzaghi consolidation problem may be generalised to hterogeneous, layered samples. The aim is to test Rhea's import data material properties with different layers and sharp gradients. Contrasting values of hydraulic conductivities are considerated
Parameter | Symbol | Value | Unit |
---|---|---|---|
Hydraulic conductivity layer 1 | k | 1.0E-4 | m/s |
Hydraulic conductivity layer 2 | k | 1.0E-8 | m/s |
The RHEA files for this scenario are found in test/tests/terzaghi_layers/
. There important files are:
-
test/tests/terzaghi_layers/Workflow_TerzaghiImportDataLayers.ipynb
. Jupyter notebook that creates the files containing the sptially-varying properties that are going to be used by RHEA. The files created areK.data
,p.data
,L.data
andG.data
. -
test/tests/terzaghi_layers/TerzaghiImportDataLayers.i
. This is the RHEA input file. Run it using therhea-opt
executable you created during compilation:../../../rhea-opt -i TerzaghiImportDataLayers.i
.
If you encounter difficulties at any step, you can ask for help on the MOOSE GitHub discussions.
von Terzaghi, K.: Die Berechnug der Durchlassigkeit des Tones aus dem Verlauf der hydromechanischen Spannungserscheinungen, Sitzungs-470ber. Akad. Wiss.(Wien). Math.-Naturwiss. Kl., Abt. Iia, 132, 125–138, 1923
Hickson, R., Barry, S., and Mercer, G.: Critical times in multilayer diffusion. Part 1: Exact solutions, International Journal of Heat and MassTransfer, 52, 5776–5783, 2009.
Paper to be added.