Linear poroelastic storage and deformation coupling
Research context
research method · conditional · As of 2026-10-10
A quasi-static poroelastic model couples elastic displacement to pore pressure and fluid storage.
Key knowledge
A quasi-static poroelastic model couples elastic displacement to pore pressure and fluid storage. Changes in volumetric strain alter fluid pressure while pressure gradients drive Darcy flux, so a rigid-aquifer storage equation is not the full deformable-medium model.
Values and equations
Sα ∂p/∂t-(κ/η) ∇^2p=-α ∂(div u)/∂t
- Sα
- Constrained storage coefficient Pa^-1
- p
- Pore-pressure change Pa
- κ
- Permeability m^2
- η
- Fluid dynamic viscosity Pa s
- α
- Biot coefficient 1
- u
- Solid displacement m
- t
- Time s
Conditions and scope
- Homogeneous isotropic small-strain linear medium with constant coefficients; declare drained/undrained and hydraulic boundaries.
- The displayed fluid equation neglects body-force gradients; anisotropy, unsaturation and stress-dependent permeability require extensions.
Sources · 1
References
Sources retain their recorded scope. A source link alone does not establish verification of every statement.
Evidence and review
Quasi-static poroelastic governing equations: Equations 1–3: displacement, storage and pore-pressure coupling (selected source body inspected).
2026-10-10 · Bounded source check of the recorded statement and conditions. This does not certify a unique physical model, reproduce the cited study or replace independent branch review.
Entry details
Permanent link to this entry ↗- Record identity
- research-earth-poroelastic-coupling
- Revision
- research.1
- Structured reference record
- Postgraduate & research reference