On the role of poroelasticity for modeling of stress fields in geothermal reservoirs
DOI10.1007/s13137-012-0032-7zbMath1254.35221OpenAlexW2025195476MaRDI QIDQ692134
Publication date: 4 December 2012
Published in: GEM - International Journal on Geomathematics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1007/s13137-012-0032-7
porous mediumboundary integral equationsstress fieldmethod of fundamental solutionsgeothermal systemsweak solution theory
Fluid-solid interactions (including aero- and hydro-elasticity, porosity, etc.) (74F10) Weak solutions to PDEs (35D30) General questions in geophysics (86A04) PDEs in connection with geophysics (35Q86)
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Cites Work
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- Mathematical methods in geothermy
- Three-dimensional modeling of heat transport in deep hydrothermal reservoirs
- Multiscale potential theory. With applications to geoscience
- Boundary integral operators for the heat equation
- On existence and uniqueness in incremental thermoelasticity
- On nonlinear Biot's consolidation models
- Efficient implementation of the MFS: The three scenarios
- The mixed problem for the Lamé system in a class of Lipschitz domains
- Model of nonlinear coupled thermo-hydro-elastodynamics response for a saturated poroelastic medium
- Dynamic behavior of saturated poroviscoelastic media
- An introduction to partial differential equations
- On singular integral equations and fundamental solutions of poroelasticity
- Diffusion in poro-elastic media
- Some existence-uniqueness results for a class of one-dimensional nonlinear Biot models
- Asymptotic Biot's models in porous media
- On the existence and the asymptotic stability of solutions to the equations of linear thermoelasticity
- A coupling of mixed and continuous Galerkin finite element methods for poroelasticity. I: The continuous in time case
- On the boundary-value problems of the theory of elasticity and Korn's inequality
- A Galerkin Method for Biot Consolidation Model
- Modeling Deep Geothermal Reservoirs: Recent Advances and Future Problems
- The existence and uniqueness theorem in Biot's consolidation theory
- Mixed boundary value problems for the Stokes system
- Continuum Theories of Mixtures: Applications
- The method of functional equations for the approximate solution of certain boundary value problems
- Application of 3D time domain boundary element formulation to wave propagation in poroelastic solids
- Trefftz method: An overview
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