Numerical modeling of two-phase flow in deformable porous media: application to CO2\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$_2$$\end{document} injection analysis in the Otway Basin, Australia

被引:0
作者
Taehyun Kim
Chan-Hee Park
Norihiro Watanabe
Eui-Seob Park
Jung-Wook Park
Yong-Bok Jung
Olaf Kolditz
机构
[1] Korea Atomic Energy Research Institute (KAERI),Nuclear Fuel Cycle and Environment Research Laboratory
[2] Korea Institute of Geoscience and Mineral Resources (KIGAM),Deep Subsurface Research Center
[3] National Institute of Advanced Industrial Science and Technology (AIST),Renewable Energy Research Center
[4] Helmholtz Centre for Environmental Research (UFZ),Environmental Informatics
[5] Applied Environmental Systems Analysis at Technical University Dresden,undefined
关键词
Two-phase flow; Capillary pressure; Hydro; Mechanical; CO; OpenGeoSys;
D O I
10.1007/s12665-021-09411-1
中图分类号
学科分类号
摘要
We examined the two-phase hydro-mechanical coupled process for subsurface applications. First, we exclusively derived governing equations for capillary pressure of the wetting fluid and pressure of the non-wetting fluid as a primary variable to make use of the global finite element model in the two-phase flow system. For the coupling process based on the derivation, we developed a module to couple the two-phase flow and the mechanical deformation for numerical modeling. For the verification of the coupling module, we solved a benchmark problem, which has an analytical solution for a single-phase hydro-mechanical system. To compare the results with those produced with the same coupling scheme of an existing module, we addressed the same benchmark problem with TOUGH–FLAC. After verification, we demonstrated the module for the two-phase hydro-mechanical coupled application of CO2\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$_2$$\end{document} storage at the field scale, the Otway Basin, Australia. The formation of caprock and reservoir in lithology had a significant effect on the movement of the CO2\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$_2$$\end{document} plume, providing a predominant pathway. Based on the mechanical analysis at the core of the CO2\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$_2$$\end{document} plume, the amount of pore pressure increase during the CO2\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$_2$$\end{document} injection period did not lead to noticeable damage in the formation.
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