Coupled Modeling of Multiphase Flow and Fault Poromechanics During Geologic CO[subscript 2] Storage

Coupling between fluid flow and mechanical deformation in porous media plays a critical role in geologic storage of CO[subscript 2] One of the key issues in simulation of CO[subscript 2] sequestration is the ability to describe the mechanical and hydraulic behavior of faults, and the influence of th...

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Main Authors: Jha, Birendra, Juanes, Ruben
Other Authors: Massachusetts Institute of Technology. Department of Civil and Environmental Engineering
Format: Article
Language:en_US
Published: Elsevier 2016
Online Access:http://hdl.handle.net/1721.1/101637
https://orcid.org/0000-0002-7370-2332
https://orcid.org/0000-0003-3855-1441
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author Jha, Birendra
Juanes, Ruben
author2 Massachusetts Institute of Technology. Department of Civil and Environmental Engineering
author_facet Massachusetts Institute of Technology. Department of Civil and Environmental Engineering
Jha, Birendra
Juanes, Ruben
author_sort Jha, Birendra
collection MIT
description Coupling between fluid flow and mechanical deformation in porous media plays a critical role in geologic storage of CO[subscript 2] One of the key issues in simulation of CO[subscript 2] sequestration is the ability to describe the mechanical and hydraulic behavior of faults, and the influence of the stress tensor and change in pressure on fault slip. Here, we present a new computational approach to model coupled multiphase flow and geomechanics of faulted reservoirs. We represent faults as surfaces embedded in a three-dimensional medium by using zero-thickness interface elements to accurately model fault slip under dynamically evolving fluid pressure and fault strength. We incorporate the effect of fluid pressures from multiphase flow in the mechanical stability of faults by defining a fault pressure. We employ a rigorous formulation of nonlinear multiphase geomechanics based on the increment in mass of fluid phases, instead of the change in porosity. Our nonlinear formulation is required to properly model systems with high compressibility or strong capillarity, as can be the case for geologic CO[subscript 2] sequestration. To account for the effect of surface stresses along fluid-fluid interfaces, we use the equivalent pore pressure in the definition of multiphase effective stress. We develop a numerical simulation tool by coupling a multiphase flow simulator with a mechanics simulator, using the unconditionally stable fixed-stress scheme for a computationally efficient sequential solution of two-way coupling between flow and geomechanics. We validate our modeling approach using several synthetic test cases that illustrate the onset and evolution of earthquakes from fluid injection.
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spelling mit-1721.1/1016372022-10-01T12:12:34Z Coupled Modeling of Multiphase Flow and Fault Poromechanics During Geologic CO[subscript 2] Storage Jha, Birendra Juanes, Ruben Massachusetts Institute of Technology. Department of Civil and Environmental Engineering Jha, Birendra Juanes, Ruben Coupling between fluid flow and mechanical deformation in porous media plays a critical role in geologic storage of CO[subscript 2] One of the key issues in simulation of CO[subscript 2] sequestration is the ability to describe the mechanical and hydraulic behavior of faults, and the influence of the stress tensor and change in pressure on fault slip. Here, we present a new computational approach to model coupled multiphase flow and geomechanics of faulted reservoirs. We represent faults as surfaces embedded in a three-dimensional medium by using zero-thickness interface elements to accurately model fault slip under dynamically evolving fluid pressure and fault strength. We incorporate the effect of fluid pressures from multiphase flow in the mechanical stability of faults by defining a fault pressure. We employ a rigorous formulation of nonlinear multiphase geomechanics based on the increment in mass of fluid phases, instead of the change in porosity. Our nonlinear formulation is required to properly model systems with high compressibility or strong capillarity, as can be the case for geologic CO[subscript 2] sequestration. To account for the effect of surface stresses along fluid-fluid interfaces, we use the equivalent pore pressure in the definition of multiphase effective stress. We develop a numerical simulation tool by coupling a multiphase flow simulator with a mechanics simulator, using the unconditionally stable fixed-stress scheme for a computationally efficient sequential solution of two-way coupling between flow and geomechanics. We validate our modeling approach using several synthetic test cases that illustrate the onset and evolution of earthquakes from fluid injection. 2016-03-09T14:46:26Z 2016-03-09T14:46:26Z 2014-12 Article http://purl.org/eprint/type/JournalArticle 18766102 http://hdl.handle.net/1721.1/101637 Jha, Birendra, and Ruben Juanes. “Coupled Modeling of Multiphase Flow and Fault Poromechanics During Geologic CO[subscript 2] Storage.” Energy Procedia 63 (2014): 3313–3329. https://orcid.org/0000-0002-7370-2332 https://orcid.org/0000-0003-3855-1441 en_US http://dx.doi.org/10.1016/j.egypro.2014.11.360 Energy Procedia Creative Commons Attribution-NonCommercial-NoDerivs License http://creativecommons.org/licenses/by-nc-nd/3.0/ application/pdf Elsevier Elsevier
spellingShingle Jha, Birendra
Juanes, Ruben
Coupled Modeling of Multiphase Flow and Fault Poromechanics During Geologic CO[subscript 2] Storage
title Coupled Modeling of Multiphase Flow and Fault Poromechanics During Geologic CO[subscript 2] Storage
title_full Coupled Modeling of Multiphase Flow and Fault Poromechanics During Geologic CO[subscript 2] Storage
title_fullStr Coupled Modeling of Multiphase Flow and Fault Poromechanics During Geologic CO[subscript 2] Storage
title_full_unstemmed Coupled Modeling of Multiphase Flow and Fault Poromechanics During Geologic CO[subscript 2] Storage
title_short Coupled Modeling of Multiphase Flow and Fault Poromechanics During Geologic CO[subscript 2] Storage
title_sort coupled modeling of multiphase flow and fault poromechanics during geologic co subscript 2 storage
url http://hdl.handle.net/1721.1/101637
https://orcid.org/0000-0002-7370-2332
https://orcid.org/0000-0003-3855-1441
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