A smoothed embedded finite-volume modeling (sEFVM) method is presented for faulted and fractured heterogeneous poroelastic media. The method casts a fully coupled strategy to treat the coupling between fault slip mechanics, deformation mechanics, and fluid flow equations. This ensures the stability and consistency of the simulation results, especially, as the fault slip is implicitly found through an iterative prediction-correction procedure. The computational grid is generated independently for embedded faults and rock matrix. The efficiency is further enhanced by extending the finite-volume discrete space by introducing only one degree of freedom per fault element. The embedded approach can lead to an oscillatory stress field at the fault...
Accurate and efficient simulation on the fluid flow and deformation in porous media is of increasing...
We apply a fully-coupled hydro-mechanical simulation tool to study fluid injection-induced pressure ...
Polygonal faults are non-tectonic fault systems which are layer-bound (at some vertical scale) and a...
A smoothed embedded finite-volume modeling (sEFVM) method is presented for faulted and fractured het...
We present a scalable collocated Finite Volume Method (FVM) to simulate induced seismicity as a resu...
We propose a multiscale finite volume method (MSFV) for simulation of coupled flow-deformation in he...
We propose a multiscale finite volume method (MSFV) for simulation of coupled flow-deformation in he...
We develop a collocated Finite Volume Method (FVM) to study induced seismicity as a result of pore p...
When modelling fluid fl ow in subsurface, the impact of solid deformation on fluid fl ow is often ov...
An increasing number of geo-energy applications require the quantitative prediction of hydromechanic...
The objective of this monograph is the derivation and implementation of a robust Finite Element form...
ABSTRACT: Faults are geological entities with thicknesses several orders of magnitude smaller than ...
Induced seismicity (earthquakes caused by injection or extraction of fluids in Earth's subsurface) i...
In Chapter 1, a finite volume-based arbitrary fracture propagation model is used to simulate fractur...
We propose a numerical method for analyzing fault slip tendency under fluid injection using the exte...
Accurate and efficient simulation on the fluid flow and deformation in porous media is of increasing...
We apply a fully-coupled hydro-mechanical simulation tool to study fluid injection-induced pressure ...
Polygonal faults are non-tectonic fault systems which are layer-bound (at some vertical scale) and a...
A smoothed embedded finite-volume modeling (sEFVM) method is presented for faulted and fractured het...
We present a scalable collocated Finite Volume Method (FVM) to simulate induced seismicity as a resu...
We propose a multiscale finite volume method (MSFV) for simulation of coupled flow-deformation in he...
We propose a multiscale finite volume method (MSFV) for simulation of coupled flow-deformation in he...
We develop a collocated Finite Volume Method (FVM) to study induced seismicity as a result of pore p...
When modelling fluid fl ow in subsurface, the impact of solid deformation on fluid fl ow is often ov...
An increasing number of geo-energy applications require the quantitative prediction of hydromechanic...
The objective of this monograph is the derivation and implementation of a robust Finite Element form...
ABSTRACT: Faults are geological entities with thicknesses several orders of magnitude smaller than ...
Induced seismicity (earthquakes caused by injection or extraction of fluids in Earth's subsurface) i...
In Chapter 1, a finite volume-based arbitrary fracture propagation model is used to simulate fractur...
We propose a numerical method for analyzing fault slip tendency under fluid injection using the exte...
Accurate and efficient simulation on the fluid flow and deformation in porous media is of increasing...
We apply a fully-coupled hydro-mechanical simulation tool to study fluid injection-induced pressure ...
Polygonal faults are non-tectonic fault systems which are layer-bound (at some vertical scale) and a...