Summarization: The present work is essentially a continuation of a previous study (Liolios and Exadaktylos, 2006) aiming at the investigation of the stress-deformation state of a porous body under the influence of mechanical and fluid flow fields, in the regions where stress singularities (e.g. cracks, thin strip inclusions, holes etc.) exist. For the solution of the problem the theories of complex variables and Cauchy-type singular integral equations are employed, since these methods are the most suitable for the calculation of the Stress Intensity Factors (SIFs) at crack tips. A fast solver has been developed for the stress analysis of multiply fractured porous media.Appearing in: Bifurcations, instabilities, degradation in geomechanic
Abstract: In this article the set of processes in the saturated porous media is considered...
International audienceDuring sedimentation, buried rocks are subjected to an increase in vertical st...
The paper deals with classical problem for cracks dislocated in a certain very specific porous elast...
The purpose of the present study is to develop a method for simultaneous solution of stress and flow...
Summarization: Complex variable representations for Dirichlet and Neumann boundary value problems of...
The objective of this monograph is the derivation and implementation of a robust Finite Element form...
Summarization: Herein a plane, steady-state fluid flow solution for fractured porous media is first ...
AbstractHerein a plane, steady-state fluid flow solution for fractured porous media is first present...
The classical theory of poroelasticity focuses on the coupled response of fluid flow and elastic def...
In Chapter 1, a finite volume-based arbitrary fracture propagation model is used to simulate fractur...
In this paper, we study the fluid flow in a deformable porous linear elastic media with a single cra...
Abstract Modeling the mechanical deformations of porous and fractured rocks requires a stress-strain...
Rock is a heterogeneous geological material. When rock is subjected to internal hydraulic pressure a...
Deep geothermal engineering is usually involved in fractured reservoirs with high permeability and b...
Modeling the mechanical deformations of porous and fractured rocks requires a stress–strain relation...
Abstract: In this article the set of processes in the saturated porous media is considered...
International audienceDuring sedimentation, buried rocks are subjected to an increase in vertical st...
The paper deals with classical problem for cracks dislocated in a certain very specific porous elast...
The purpose of the present study is to develop a method for simultaneous solution of stress and flow...
Summarization: Complex variable representations for Dirichlet and Neumann boundary value problems of...
The objective of this monograph is the derivation and implementation of a robust Finite Element form...
Summarization: Herein a plane, steady-state fluid flow solution for fractured porous media is first ...
AbstractHerein a plane, steady-state fluid flow solution for fractured porous media is first present...
The classical theory of poroelasticity focuses on the coupled response of fluid flow and elastic def...
In Chapter 1, a finite volume-based arbitrary fracture propagation model is used to simulate fractur...
In this paper, we study the fluid flow in a deformable porous linear elastic media with a single cra...
Abstract Modeling the mechanical deformations of porous and fractured rocks requires a stress-strain...
Rock is a heterogeneous geological material. When rock is subjected to internal hydraulic pressure a...
Deep geothermal engineering is usually involved in fractured reservoirs with high permeability and b...
Modeling the mechanical deformations of porous and fractured rocks requires a stress–strain relation...
Abstract: In this article the set of processes in the saturated porous media is considered...
International audienceDuring sedimentation, buried rocks are subjected to an increase in vertical st...
The paper deals with classical problem for cracks dislocated in a certain very specific porous elast...