Record Details

Title Physical/Computational Framework for EGS In Situ Fracture Stimulation
Authors Justin Pogacnik, Peter Leary and Peter Malin
Year 2012
Conference New Zealand Geothermal Workshop
Keywords Fully coupled finite element model, deformable porous media, Engineered/Enhanced Geothermal Systems, heat and mass transfer, permeability enhancement, power-law scaling.
Abstract We employ a fully coupled finite element analysis of a thermal, hydraulic, and mechanical (THM) energy scheme to simulate stress/strain damage induced in an in situ poroperm medium stressed by wellbore fluid pressurization in the medium. Our poroperm medium is characterized by two empirical constraints: (i) a normally-populated fracture-density distribution that percolates fluid via long-range spatially correlated grain-scale fracture connectivity at all scale; and (ii) a (potentially) long-tailed (‘lognormal’) permeability distribution ê associated with percolation pathways related to normally distributed porosity distribution F expressed by ê = ê0exp(á(ö-ö0)) as attested by clastic reservoir well-core poroperm fluctuation systematics. The degree of fracture connectivity in such a medium is parameterized by á = ratio of standard deviations of logê and ö distributions. Small values of á describe low degrees of fracture connectivity and hence low bulk permeability, while large values of á describe high degrees of fracture connectivity giving high bulk permeability. Wellbore fluid pressurization creates shear strains in the fracture-heterogeneous poroperm medium, putatively generating grain-scale fracture damage additional to the pre-existing grain-scale fracture damage in the medium. Injecting grain-scale fracture damage can be seen as creating new fluid flow pathways and increased bulk permeability via newly created grain-scale fracture-connectivity. Pressure-induced fracture damage injection thus leads to greater fluid permeability equivalent to incrementing the value of the fracture-connectivity parameter á. Such wellbore pressurization could be conducted in interest of flow stimulation of an inter-wellbore EGS heat exchange volume.
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