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Poroelasticity is a field in materials science and mechanics that studies the interaction between fluid flow, pressure and bulk solid deformation within a linear porous medium and it is an extension of elasticity and porous medium flow (diffusion equation). Pore pressure, storage, and undrained coefficients are also introduced and useful relations are proven. The basic principles of the theory of poroelasticity are twofold

This Motherless Land by Nikki May - Penguin Books Australia

The equations of equilibrium of the porous medium, and the equations of conservation of mass of the two components Characterizing poroelasticity can provide insight into a broad range of physiological functions, and is done qualitatively in the clinic by palpation. The solids and the pore fluid.

This book provides an excellent introduction to linear poroelasticity and is especially relevant to those involved in civil engineering, petroleum and reservoir engineering, rock mechanics, hydrology, geophysics, and biomechanics.

Poroelasticity theory describes the interaction between fluid flow and deformation in elastic porous media This bidirectional multiphysics coupling relates fluid flow and solid deformation with linear constitutive relations. There are two major parts for poroelasticity The static poroelasticity accounts for a process in which water movement and solid skeleton deformation occur simultaneously and affect each other.