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dc.contributor.advisorRuben Juanes.en_US
dc.contributor.authorJha, Birendra, Ph. D. Massachusetts Institute of Technology. Department of Civil and Environmental Engineeringen_US
dc.contributor.otherMassachusetts Institute of Technology. Department of Civil and Environmental Engineering.en_US
dc.date.accessioned2014-07-11T21:08:23Z
dc.date.available2014-07-11T21:08:23Z
dc.date.copyright2013en_US
dc.date.issued2014en_US
dc.identifier.urihttp://hdl.handle.net/1721.1/88391
dc.descriptionThesis: Ph. D., Massachusetts Institute of Technology, Department of Civil and Environmental Engineering, February, 2014.en_US
dc.descriptionCataloged from PDF version of thesis.en_US
dc.descriptionIncludes bibliographical references (pages 153-172).en_US
dc.description.abstractEnhanced oil recovery by displacing oil with solvents such as carbon dioxide requires development of miscibility between the two fluids to maximize the displacement efficiency. Prevention of inadvertent triggering of earthquakes due to injection or production of fluids in the underground requires understanding of coupling between flow and deformation processes. In this Dissertation, we study flow through porous media in two different contexts: effect of viscosity on mixing of fluids, and triggering of earthquakes due to coupling between flow and deformation. We show that miscible viscous fingering-the hydrodynamic instability that arises when a less viscous fluid displaces the more viscous one-can be employed as an agent for enhanced mixing in porous media flows. Based on results from high-resolution numerical simulations, we derive a macroscopic model of mixing that captures the delicate interplay between channeling of less viscous fluid and creation of interfacial area as a result of viscous fingering. The coupling between subsurface flow and geomechanical deformation is critical in the assessment of the environmental impacts of groundwater use, underground liquid waste disposal, geologic carbon dioxide storage, and exploitation of shale gas reserves. 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, and employ a rigorous formulation of nonlinear multiphase geomechanics that is capable of handling strong capillary effects. We develop a numerical simulation tool by coupling a multiphase flow simulator with a mechanics simulator, using the unconditionally stable fixed-stress operator split for the sequential solution of two-way coupling between flow and geomechanics. We validate our modeling approach using test cases that illustrate the onset and evolution of earthquakes from fluid injection and production.en_US
dc.description.statementofresponsibilityby Birendra Jha.en_US
dc.format.extent172 pagesen_US
dc.language.isoengen_US
dc.publisherMassachusetts Institute of Technologyen_US
dc.rightsM.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission.en_US
dc.rights.urihttp://dspace.mit.edu/handle/1721.1/7582en_US
dc.subjectCivil and Environmental Engineering.en_US
dc.titleFlow through porous media : from mixing of fluids to triggering of earthquakesen_US
dc.title.alternativeFrom mixing of fluids to triggering of earthquakesen_US
dc.typeThesisen_US
dc.description.degreePh. D.en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Civil and Environmental Engineering
dc.identifier.oclc881691213en_US


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