We present a scalable collocated Finite Volume Method (FVM) to simulate induced seismicity as a result of pore pressure changes. A discrete system is obtained based on a fully-implicit fully-coupled description of flow, elastic deformation, and contact mechanics at fault surfaces on a flexible unstructured mesh. The cell-centered collocated scheme leads to a convenient integration of the different physical equations, as the unknowns share the same discrete locations on the mesh. Additionally, a generic multi-point flux approximation is formulated to treat heterogeneity, anisotropy, and cross-derivative terms for both flow and mechanics equations. The resulting system, though flexible and accurate, can lead to excessive computational costs f...
We present a 2-D multi-block method for earthquake rupture dynamics in complex geometries using summ...
We develop a stable and high-order accurate finite difference method for problems in earthquake rupt...
A major goal in earthquake physics is to derive a constitutive framework for fault slip that capture...
We develop a collocated Finite Volume Method (FVM) to study induced seismicity as a result of pore p...
An increasing number of geo-energy applications require the quantitative prediction of hydromechanic...
A smoothed embedded finite-volume modeling (sEFVM) method is presented for faulted and fractured het...
We propose a multiscale finite volume method (MSFV) for simulation of coupled flow-deformation in he...
We couple a node-centered finite volume method to a high order finite dif- ference method to simulat...
We propose a multiscale finite volume method (MSFV) for simulation of coupled flow-deformation in he...
We couple a node-centered finite volume method to a high order finite difference method to simulate ...
Induced seismicity (earthquakes caused by injection or extraction of fluids in Earth's subsurface) i...
When modelling fluid fl ow in subsurface, the impact of solid deformation on fluid fl ow is often ov...
ABSTRACT: Faults are geological entities with thicknesses several orders of magnitude smaller than ...
Coupling between fluid flow and mechanical deformation in porous media plays a critical role in geol...
Modelling dynamic rupture is essential to correctly describe the process of induced seismicity. Defm...
We present a 2-D multi-block method for earthquake rupture dynamics in complex geometries using summ...
We develop a stable and high-order accurate finite difference method for problems in earthquake rupt...
A major goal in earthquake physics is to derive a constitutive framework for fault slip that capture...
We develop a collocated Finite Volume Method (FVM) to study induced seismicity as a result of pore p...
An increasing number of geo-energy applications require the quantitative prediction of hydromechanic...
A smoothed embedded finite-volume modeling (sEFVM) method is presented for faulted and fractured het...
We propose a multiscale finite volume method (MSFV) for simulation of coupled flow-deformation in he...
We couple a node-centered finite volume method to a high order finite dif- ference method to simulat...
We propose a multiscale finite volume method (MSFV) for simulation of coupled flow-deformation in he...
We couple a node-centered finite volume method to a high order finite difference method to simulate ...
Induced seismicity (earthquakes caused by injection or extraction of fluids in Earth's subsurface) i...
When modelling fluid fl ow in subsurface, the impact of solid deformation on fluid fl ow is often ov...
ABSTRACT: Faults are geological entities with thicknesses several orders of magnitude smaller than ...
Coupling between fluid flow and mechanical deformation in porous media plays a critical role in geol...
Modelling dynamic rupture is essential to correctly describe the process of induced seismicity. Defm...
We present a 2-D multi-block method for earthquake rupture dynamics in complex geometries using summ...
We develop a stable and high-order accurate finite difference method for problems in earthquake rupt...
A major goal in earthquake physics is to derive a constitutive framework for fault slip that capture...