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International Journal of Rock Mechanics & Mining Sciences 39 (2002) 429-442. 指導教授 : 陳瑞昇、董家鈞 老師 學生 : 楊慶中 日期 :99.12.30. A MODELING APPROACH FOR ANALYSIS OF COUPLED MULTIPHASE FLUID FLOW , HEAT TRANSFER, AND DEFORMATION IN FRACTURED POROUS ROCK. J. Rutqvist ,Y.-S. Wu , C.-F Tsang , G. Bodvarsson.
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International Journal of Rock Mechanics & Mining Sciences 39 (2002) 429-442 指導教授:陳瑞昇、董家鈞 老師 學生:楊慶中 日期:99.12.30 A MODELING APPROACH FOR ANALYSIS OF COUPLED MULTIPHASE FLUID FLOW , HEAT TRANSFER, AND DEFORMATION IN FRACTURED POROUS ROCK J. Rutqvist ,Y.-S. Wu , C.-F Tsang , G. Bodvarsson 1
Outline • Introduction • FLAC3D • TOUGH2 • Coupling module • Examples Results • Conclusion 2
Introduction • Coupled thermal–hydrologic–mechanical processes under multiphase flow conditions are prevalent in geoscientific applications. • A few of the most important include nuclear waste disposal in geological media, deep underground injection of hazardous wasteand underground storage of carbon dioxide into permeable aquifers. 3
Introduction • However, there is no single computer code that handles general coupled thermal–hydrologic–mechanical processes . • The two codes—TOUGH2 and FLAC3D are linked using sequential execution and data transfer through nonlinear coupling functions. 4
FLAC3D 5
FLAC3D • FALC (Fast Lagrangian Analysis of Continua ), the finite difference code is developed by the United States Itasca Consulting Group Inc in 1986 ,and FLAC3D developed in 1994. • Code is developed for rock and soil mechanics and can also handle thermomechanical and hydromechanical problem for single-phase fluid flow. 6
FLAC3D Motion equations Cauchy’s fomula 7
TOUGH2 9
TOUGH2 • TOUGH(Transport of Unsaturanted Groundwater and Heat) developed in the Earth Sciences Division of Lawrence Berkeley National Laboratory in 1987. • TOUGH2 is a simulator for multiphase, multicomponent , non-isothermal flows in fractured-porous media. 10
TOUGH2 Governing equations 11
Conclusion • We have linked two codes—TOUGH2 and FLAC3D—for analysis of coupled thermal-hydrologic-mechanical processes. • The coupling modules contain nonlinear stress versus permeability functions.
Conclusion • In both these examples, the hydromechanical changes are relatively slow, which is most suitable for the sequentially explicit solution. • Problems with higher strain rates relative to fluid mobility may require the sequential implicit approach or ultimately a fully implicit coupledapproach.