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Dynamics of hydrofracturing and permeability evolution in layered reservoirs

2015

International audience; A coupled hydro-mechanical model is presented to model fluid driven fracturing in layered porous rocks. In the model the solid elastic continuum is described by a discrete element approach coupled with a fluid continuum grid that is used to solve Darcy based pressure diffusion. The model assumes poro-elasto-plastic effects and yields real time dynamic aspects of the fracturing and effective stress evolution under the influence of excess fluid pressure gradients. We show that the formation and propagation of hydrofractures are sensitive to mechanical and tectonic conditions of the system. In cases where elevated fluid pressure is the sole driving agent in a stable tec…

reservoir[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]Materials Science (miscellaneous)Effective stressfluid pressureBiophysicsGeneral Physics and AstronomyPattern formation[SDU.STU]Sciences of the Universe [physics]/Earth Sciencesreservoirsstresshydrofracturesfluid pressure4Ultimate tensile strength[PHYS.MECA.SOLID]Physics [physics]/Mechanics [physics]/Solid mechanics [physics.class-ph][PHYS.MECA.MEFL]Physics [physics]/Mechanics [physics]/Fluid mechanics [physics.class-ph]Physical and Theoretical ChemistryPorosityMathematical PhysicsCauchy stress tensorPhysicsMechanicssimulationreservoirs2lcsh:QC1-999TectonicsPermeability (earth sciences)Keywords: hydrofractures1simulation3Relative permeabilityhydrofractureGeologystress5lcsh:Physics
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