Two-phase porous media flow: Strange pressure field #17049
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Hi MOOSE Porous media team I am now testing a simple 2D CO2 injection problem (coupled with mechanics and with gravity effect on) based on the "modules/porous_flow/examples/thm_example/2D.i" example. The model simply has an aquifer with a high permeability (1e-12 m2) between upper caprock and bottom both with low permeability (1e-19 m2). As expected, while CO2 injection, under bouncy forces, the CO2 plume gradually moves to upper regions on in the aquifer. However, the strange thing is in the change of fluid pressure field, which is much large in the caprock than expected. Could you help me point out the problem? Thank you. (The pressure change (to the hydrostatic pressure) is denoted "pgas2". ) |
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Replies: 5 comments 10 replies
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No answer, just some questions
a |
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Andy, thank you again for the help. I find, as your suggested way, after load and initialize strain using the output of a previous run (already reached steady state), there are still gradual changes in displacement (and strain and stress) always ( since run even after a very long time run) while without fluid injection. Could you help me point out the problem. The file link. Best, Yi Zhang |
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By viewing using Paraview, I find the gradual changes in displacement (or strain, pressure) occur at the transition between the high-permeability aquifer zone and low-permeability zones. The reason is still unknow. Perhaps the error comes from the physics setting some where. I have not found the improper setting. I will try Controls system. Thanks! |
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I had tested another whole day today, but still cannot work out the problem. Is there a two-phase flow mechanical coupled problem with first gravity equilibrium? (I wish). Thank you. |
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Andy, thank you very much for your help! |
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No answer, just some questions
PorousFlowEffectiveStressCoupling
Kernel fordisp_z
?a