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dc.contributor.advisorGhassemi, Ahmad
dc.creatorLee, Byungtark
dc.date.accessioned2011-10-21T22:04:01Z
dc.date.accessioned2011-10-22T07:12:11Z
dc.date.available2011-10-21T22:04:01Z
dc.date.available2011-10-22T07:12:11Z
dc.date.created2011-08
dc.date.issued2011-10-21
dc.date.submittedAugust 2011
dc.identifier.urihttps://hdl.handle.net/1969.1/ETD-TAMU-2011-08-10100
dc.description.abstractIn geothermal reservoirs and unconventional gas reservoirs with very low matrix permeability, fractures are the main routes of fluid flow and heat transport, so the fracture permeability change is important. In fact, reservoir development under this circumstance relies on generation and stimulation of a fracture network. This thesis presents numerical simulation of the response of a fractured rock to injection and extraction considering the role of poro-thermoelasticity and joint deformation. Fluid flow and heat transport in the fracture are treated using a finite difference method while the fracture and rock matrix deformation are determined using the displacement discontinuity method (DDM). The fractures response to fluid injection and extraction is affected both by the induced stresses as well as by the initial far-field stress. The latter is accounted for using the non-equilibrium condition, i.e., relaxing the assumption that the rock joints are in equilibrium with the in-situ stress state. The fully coupled DDM simulation has been used to carry out several case studies to model the fracture response under different injection/extractions, in-situ stresses, joint geometries and properties, for both equilibrium and non-equilibrium conditions. The following observations are made: i) Fluid injection increases the pressure causing the joint to open. For non-isothermal injection, cooling increases the fracture aperture drastically by inducing tensile stresses. Higher fracture aperture means higher conductivity. ii) In a single fracture under constant anisotropic in-situ stress (non-equilibrium condition), permanent shear slip is encountered on all fracture segments when the shear strength is overcome by shear stress in response to fluid injection. With cooling operation, the fracture segments in the vicinity of the injection point are opened due to cooling-induced tensile stress and injection pressure, and all the fracture segments experience slip. iii) Fluid pressure in fractures increases in response to compression. The fluid compressibility and joint stiffness play a role. iv) When there are injection and extraction in fractured reservoirs, the cooler fluid flows through the fracture channels from the injection point to extraction well extracting heat from the warmer reservoir matrix. As the matrix cools, the resulting thermal stress increases the fracture apertures and thus increases the fracture conductivity. v) Injection decreases the amount of effective stress due to pressure increase in fracture and matrix near a well. In contrast, extraction increases the amount of effective stress due to pressure drop in fracture and matrix.en
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.subjectGeomechanicsen
dc.subjectNumerical Simulationen
dc.subjectPetroleum Engineeringen
dc.subjectNumerical Investigationen
dc.subjectEnhanced Geothermal System (EGS)en
dc.subjectNaturally Fractured Reservoiren
dc.subjectPermeabilityen
dc.subjectFracture apertureen
dc.subjectInjection/Extractionen
dc.subjectDisplacement Discontinuity Method (DDM)en
dc.subjectFinite Difference Method FDM)en
dc.titleNumerical Investigation of Fractured Reservoir Response to Injection/Extraction Using a Fully Coupled Displacement Discontinuity Methoden
dc.typeThesisen
thesis.degree.departmentPetroleum Engineeringen
thesis.degree.disciplinePetroleum Engineeringen
thesis.degree.grantorTexas A&M Universityen
thesis.degree.nameMaster of Scienceen
thesis.degree.levelMastersen
dc.contributor.committeeMemberHolditch, Stephen A.
dc.contributor.committeeMemberDuan, Benchun
dc.type.genrethesisen
dc.type.materialtexten


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