wg:magma_migration:benchmark:start
Differences
This shows you the differences between two versions of the page.
| Both sides previous revision Previous revision Next revision | Previous revision | ||
|
wg:magma_migration:benchmark:start [2014/11/04 22:47] ljhwang [Model descriptions] |
wg:magma_migration:benchmark:start [2020/12/29 23:25] (current) ljhwang |
||
|---|---|---|---|
| Line 1: | Line 1: | ||
| ====== Benchmarks ====== | ====== Benchmarks ====== | ||
| + | |||
| + | //This content has been moved to hubzero. LJ Hwang 2020.12.29// | ||
| Benchmarks for the Magma Dynamics Demonstration Suite (MADDs). | Benchmarks for the Magma Dynamics Demonstration Suite (MADDs). | ||
| Line 144: | Line 146: | ||
| and then repeating the procedures detailed above for the 2D system. The initial condition, read in from the file ./input/solitaryWaves3DGlobal.dat, is that of a single 1D solitary wave in the vertical direction set against a noisy background distribution which evolves with time into a set of 3D solitary waves. | and then repeating the procedures detailed above for the 2D system. The initial condition, read in from the file ./input/solitaryWaves3DGlobal.dat, is that of a single 1D solitary wave in the vertical direction set against a noisy background distribution which evolves with time into a set of 3D solitary waves. | ||
| - | //upload file - 2D Solitary Wave. | + | //2D Solitary Wave. |
| A 2D solitary wave with a wave speed of 7 rising through a solid with a constant speed of -2. The wave shows no visible diffusive behavior.// | A 2D solitary wave with a wave speed of 7 rising through a solid with a constant speed of -2. The wave shows no visible diffusive behavior.// | ||
| - | + | {{ :wg:magma_migration:benchmark:2d_solitary_wave.png?100 |}} | |
| - | //upload file - Noisy 1D Solitary Wave Initial Condition. | + | // Noisy 1D Solitary Wave Initial Condition. |
| Initial condition of a vertically changing 1D solitary wave with a certain amount of introduced noise, which allows 2D solitary waves to emerge over time.// | Initial condition of a vertically changing 1D solitary wave with a certain amount of introduced noise, which allows 2D solitary waves to emerge over time.// | ||
| - | + | {{ :wg:magma_migration:benchmark:1d_solitary_wave.jpeg?100 |}} | |
| - | //upload file - Emerging 2D Solitary Waves. | + | // Emerging 2D Solitary Waves. |
| Solitary waves emerging from a noisy 1D solitary wave initial condition.// | Solitary waves emerging from a noisy 1D solitary wave initial condition.// | ||
| - | + | {{ :wg:magma_migration:benchmark:2d_solitary_wave_emerging.jpeg?100 |}} | |
| - | //upload file - Emergent 2D Solitary Waves. | + | // Emergent 2D Solitary Waves. |
| Solitary waves having emerged from a noisy 1D solitary wave initial distribution.// | Solitary waves having emerged from a noisy 1D solitary wave initial distribution.// | ||
| - | + | {{ :wg:magma_migration:benchmark:2d_solitary_wave_emerging_noisy.jpeg?100 |}} | |
| - | //upload file - Emergent 3D Solitary Waves. | + | //{{ :wg:magma_migration:benchmark:3d_solitary_wave_emerging.png?100 |}}Emergent 3D Solitary Waves. |
| 3D Solitary Waves emerging from a noisy 1D Solitary Wave initial distribution// | 3D Solitary Waves emerging from a noisy 1D Solitary Wave initial distribution// | ||
| Line 180: | Line 182: | ||
| Some images for the x and y velocity components, the dynamic and compaction pressures, the porosity, the melt fraction and the x and y melt velocity components are attached below. | Some images for the x and y velocity components, the dynamic and compaction pressures, the porosity, the melt fraction and the x and y melt velocity components are attached below. | ||
| - | //upload file - Isoviscous McKenzie System with Corner Flow BC - 1. | + | //Isoviscous McKenzie System with Corner Flow BC - 1. |
| After 1 time step// | After 1 time step// | ||
| - | + | {{ :wg:magma_migration:benchmark:iso_bc-1.png?100 |}} | |
| - | //upload file - Isoviscous McKenzie System with Corner Flow BC - 50. | + | //Isoviscous McKenzie System with Corner Flow BC - 50. |
| After 50 time steps// | After 50 time steps// | ||
| - | + | {{ :wg:magma_migration:benchmark:iso_bc-50.png?100 |}} | |
| - | //upload file - Isoviscous McKenzie System with Corner Flow BC - 3200. | + | //Isoviscous McKenzie System with Corner Flow BC - 3200. |
| After 3200 time steps.// | After 3200 time steps.// | ||
| - | + | {{ :wg:magma_migration:benchmark:iso_bc-3200.png?100 |}} | |
| - | //upload file - Velocity - x component. | + | //Velocity - x component. |
| x component of the velocity field for the 3D isoviscous McKenzie model with ridge BCs at time step 150.// | x component of the velocity field for the 3D isoviscous McKenzie model with ridge BCs at time step 150.// | ||
| - | + | {{ :wg:magma_migration:benchmark:velocity_x.png?100 |}} | |
| - | //upload file - Velocity - y component. | + | // Velocity - y component. |
| y component of the velocity field for the 3D isoviscous McKenzie model with ridge BCs at time step 150.// | y component of the velocity field for the 3D isoviscous McKenzie model with ridge BCs at time step 150.// | ||
| - | + | {{ :wg:magma_migration:benchmark:velocity_y.png?100 |}} | |
| - | //upload file -Dynamic (Stokes) pressure, | + | //Dynamic (Stokes) pressure, |
| Dynamic pressure due to viscous shear for the 3D isoviscous McKenzie model with ridge BCs at time step 150.// | Dynamic pressure due to viscous shear for the 3D isoviscous McKenzie model with ridge BCs at time step 150.// | ||
| - | + | {{ :wg:magma_migration:benchmark:dynamic_pressure.png?100 |}} | |
| - | //upload file - Porosity. | + | //Porosity. |
| Porosity field for the 3D isoviscous McKenzie model with ridge BCs at time step 150.// | Porosity field for the 3D isoviscous McKenzie model with ridge BCs at time step 150.// | ||
| - | + | {{ :wg:magma_migration:benchmark:porosity_bc150.png?100 |}} | |
| - | //upload file - Compaction pressure. | + | //Compaction pressure. |
| Compaction pressure due to compressibility of the solid phase for the 3D isoviscous McKenzie model with ridge BCs at time step 150.// | Compaction pressure due to compressibility of the solid phase for the 3D isoviscous McKenzie model with ridge BCs at time step 150.// | ||
| - | + | {{ :wg:magma_migration:benchmark:compaction_pressure.png?100 |}} | |
| - | //upload file - Melt fraction. | + | //Melt fraction. |
| Melt fraction field representing the melt to solid phase of the 3D isoviscous McKenzie model with ridge BCs at time step 150.// | Melt fraction field representing the melt to solid phase of the 3D isoviscous McKenzie model with ridge BCs at time step 150.// | ||
| - | + | {{ :wg:magma_migration:benchmark:melt_fraction.png?100 |}} | |
| - | //upload file - Melt velocity - x component. | + | //Melt velocity - x component. |
| x component of the melt velocity field for the 3D isoviscous McKenzie model with ridge BCs at time step 150.// | x component of the melt velocity field for the 3D isoviscous McKenzie model with ridge BCs at time step 150.// | ||
| - | + | {{ :wg:magma_migration:benchmark:melt_velocity_x.png?100 |}} | |
| - | //upload file -Melt velocity - y component. | + | //Melt velocity - y component. |
| y component of the Melt velocity field for the 3D isoviscous McKenzie model with ridge BCs at time step 150.// | y component of the Melt velocity field for the 3D isoviscous McKenzie model with ridge BCs at time step 150.// | ||
| + | {{ :wg:magma_migration:benchmark:melt_velocity_y.png?100 |}} | ||
wg/magma_migration/benchmark/start.1415141267.txt.gz · Last modified: 2014/11/04 22:47 by ljhwang
Page Tools
Except where otherwise noted, content on this wiki is licensed under the following license: CC Attribution-Share Alike 3.0 Unported
