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Biot theory of poroelasticity

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This document verifies that groundwater flow principles are correctly implemented in PLAXIS. Poroelasticity theory, first introduced by Biot (1941), counts for coupled hydro-mechanical processes. The presented verification example studies the case of a drilled vertical borehole in saturated soil formation (porous rock), subjected to non-hydrostatic in situ stress. PLAXIS results are compared to the analytical solution provided by Detournay & Cheng (1988).

Used version:

  • PLAXIS 2D - Version 2015.02
  • PLAXIS 3D - Anniversary Edition (AE.01)

This requires a PlaxFlow module for groundwater flow

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Plx_Verification_Biot_theory_of_poroelasticity[2015].pdfValidation description, version: PLAXIS 2D 2015 and PLAXIS 3D AEpdf| 1.75 MB
Plx_Verification_Biot_theory_of_poroelasticity[2D2015.02].p2dxlogCommand log file for PLAXIS 2D 2015 to create the model. Use 'Save as' and load it in the Commands Runnerother| 4.34 KB
Plx_Verification_Biot_theory_of_poroelasticity[3DAE.01].p3dlogCommand log file for PLAXIS 3D AE to create the model. Use 'Save as' and load it in the Commands Runnerother| 5.05 KB

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