Hydromechanical modeling of solid deformation and fluid flow in the transversely isotropic fissured rocks
Geomaterials containing fissures such as some sedimentary rocks often exhibit a bimodal pore size distribution, and they are also inherently anisotropic due to the distinct bedding planes. Hydromechanical modeling of solid deformation and fluid flow of such geomaterials remains a significant challen...
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| Published in | Computers and geotechnics Vol. 128; p. 103812 |
|---|---|
| Main Author | |
| Format | Journal Article |
| Language | English |
| Published |
New York
Elsevier Ltd
01.12.2020
Elsevier BV |
| Subjects | |
| Online Access | Get full text |
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| Abstract | Geomaterials containing fissures such as some sedimentary rocks often exhibit a bimodal pore size distribution, and they are also inherently anisotropic due to the distinct bedding planes. Hydromechanical modeling of solid deformation and fluid flow of such geomaterials remains a significant challenge. In this paper, we have developed a unique anisotropic double porosity elastoplastic framework to describe such processes. Furthermore, for the solid constitutive model, because of the loss of stress tensor coaxiality between the trial state and the final state, we have derived a new implicit return mapping algorithm to obtain the updated effective stress, history parameters and consistent tangent operator for any given strain increment efficiently, followed by a uniaxial strain point simulation to provide benchmark results. Subsequently, 3D stress point simulations are carried out to calibrate the projection and plasticity parameters using triaxial experimental data as well as to illustrate the strain-softening phenomenon. Initial boundary value problem simulations have been conducted to analyze the impacts of fluid flow and solid constitutive model on the resulting geomaterials’ responses. The overarching goal of this paper is to better understand the coupled solid deformation-fluid flow in the transversely isotropic fissured rocks. |
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| AbstractList | Geomaterials containing fissures such as some sedimentary rocks often exhibit a bimodal pore size distribution, and they are also inherently anisotropic due to the distinct bedding planes. Hydromechanical modeling of solid deformation and fluid flow of such geomaterials remains a significant challenge. In this paper, we have developed a unique anisotropic double porosity elastoplastic framework to describe such processes. Furthermore, for the solid constitutive model, because of the loss of stress tensor coaxiality between the trial state and the final state, we have derived a new implicit return mapping algorithm to obtain the updated effective stress, history parameters and consistent tangent operator for any given strain increment efficiently, followed by a uniaxial strain point simulation to provide benchmark results. Subsequently, 3D stress point simulations are carried out to calibrate the projection and plasticity parameters using triaxial experimental data as well as to illustrate the strain-softening phenomenon. Initial boundary value problem simulations have been conducted to analyze the impacts of fluid flow and solid constitutive model on the resulting geomaterials’ responses. The overarching goal of this paper is to better understand the coupled solid deformation-fluid flow in the transversely isotropic fissured rocks. |
| ArticleNumber | 103812 |
| Author | Zhang, Qi |
| Author_xml | – sequence: 1 givenname: Qi orcidid: 0000-0002-4637-6308 surname: Zhang fullname: Zhang, Qi email: qzhang94@stanford.edu organization: Department of Civil and Environmental Engineering, Stanford University, Stanford, CA 94305, USA |
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| Keywords | Transverse isotropy Strain localization Elastoplasticity Double porosity Coupled formulation Return mapping algorithm |
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| SubjectTerms | Algorithms Anisotropy Boundary value problems Computational fluid dynamics Constitutive models Coupled formulation Deformation Double porosity Elastoplasticity Fluid flow Geomaterials Mathematical models Modelling Parameters Pore size Pore size distribution Porosity Return mapping algorithm Sedimentary rocks Simulation Size distribution Strain Strain localization Tensors Transverse isotropy |
| Title | Hydromechanical modeling of solid deformation and fluid flow in the transversely isotropic fissured rocks |
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