Biot theory of poroelasticity


Application PLAXIS 2D
PLAXIS 3D
Version PLAXIS 2D
PLAXIS 3D
Date created 30 June 2016
Date modified 30 June 2016

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:


 This requires a PlaxFlow module for groundwater flow

 

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