A three-dimensional integral equation model for calculating poro- and thermoelastic stresses induced by cold water injection into a geothermal reservoir

DOI10.1002/nag.780zbMath1273.74196OpenAlexW2036986201MaRDI QIDQ2854675

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Publication date: 24 October 2013

Published in: International Journal for Numerical and Analytical Methods in Geomechanics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1002/nag.780

zbMATH Keywords

thermoelastic stressdisplacement discontinuitygeothermal energyporoelastic stressreservoir seismicity

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Fluid-solid interactions (including aero- and hydro-elasticity, porosity, etc.) (74F10) Flows in porous media; filtration; seepage (76S05) Geophysical solid mechanics (74L05)

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Efficient numerical solution of the volume integro-differential equation for time-varying temperature fields in heterogeneous media ⋮ DDFS\(^{\text{3D}}\): a set of open-source codes leveraging hybrid 3D displacement discontinuity method and fictitious stress method to simulate fractures ⋮ Analysis of thermal effect around an underground storage cavern with a combined three-dimensional indirect boundary element method

Cites Work

• Streamline upwind/Petrov-Galerkin formulations for convection dominated flows with particular emphasis on the incompressible Navier-Stokes equations
• On singular integral equations and fundamental solutions of poroelasticity
• A time domain boundary element method for poroelasticity
• Integral equation solution of heat extraction-induced thermal stress in enhanced geothermal reservoirs
• An ‘upwind’ finite element scheme for two‐dimensional convective transport equation
• An integral equation solution for three-dimensional heat extraction from planar fracture in hot dry rock

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