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Journal ArticleDOI

Poroelasticity equations derived from microstructure

Robert Burridge, +1 more
- 01 Oct 1981 - 
- Vol. 70, Iss: 4, pp 1140-1146
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TLDR
In this paper, the linear macroscopic mechanical behavior of a porous elastic solid saturated with a compressible viscous fluid is derived based on the equations of linear elasticity in the solid, the linearized Navier-Stokes equations in the fluid, and appropriate conditions at the solid-fluid boundary.
Abstract
Equations are derived which govern the linear macroscopic mechanical behavior of a porous elastic solid saturated with a compressible viscous fluid. The derivation is based on the equations of linear elasticity in the solid, the linearized Navier–Stokes equations in the fluid, and appropriate conditions at the solid–fluid boundary. The scale of the pores is assumed to be small compared to the macroscopic scale, so that the two‐space method of homogenization can be used to deduce the macroscopic equations. When the dimensionless viscosity of the fluid is small, the resulting equations are those of Biot, who obtained them by hypothesizing the form of the macroscopic constitutive relations. The present derivation verifies those relations, and shows how the coefficients in them can be calculated, in principle, from the microstructure. When the dimensionless viscosity is of order one, a different equation is obtained, which is that of a viscoelastic solid.

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Journal ArticleDOI

Dynamic poroelasticity: A unified model with the squirt and the Biot mechanisms

TL;DR: In this article, the velocity dispersion and attenuation of seismic and acoustic waves in rocks with fluids are affected by the two most important modes of fluid/solid interaction: (1) the Biot mechanism where the fluid is forced to participate in the solid's motion by viscous friction and inertial coupling, and (2) the squirt-flow mechanism where fluid is squeezed out of thin pores deformed by a passing wave.
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Wave propagation simulation in a linear viscoacoustic medium

TL;DR: In this article, the Boltzmann superposition principle based on the general standard linear solid rheology is implemented in the equation of motion by the introduction of memory variables, and the propagation in time is done by a direct expansion of the evolution operator by a Chebycheff polynomial series.
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Acoustic relaxation in sedimentary rocks; dependence on grain contacts and fluid saturation

TL;DR: In this article, a model based on observed microstructures in sandstones is proposed to predict the real and imaginary parts of the complex frame moduli as a function of frequency and fluid saturation.
Journal ArticleDOI

The mechanical properties of materials with interconnected cracks and pores

TL;DR: In this article, the effect on the overall properties of a cracked solid of the existence of connections between otherwise isolated cracks and of small-scale porosity within the solid material was investigated.