Simulations of T-intersections with dead-end fractures demonstrate that density- or pressure-driven flow inside the dead-end branch enhances heat transfer to the rock matrix by sustaining larger temperature differences.
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2 Pith papers cite this work. Polarity classification is still indexing.
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A calibrated multiphase flow-geomechanics model of the Wilmington Oil Field from 1936-2020 indicates that initializing the sedimentary section with low deviatoric stress provides the best fit to historical ground deformation data and implies a shift from the previously assumed reverse-faulting regim
citing papers explorer
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Enhanced Heat Transfer through Density- and Pressure-Driven Flow at Fracture Intersections With Dead-Ends
Simulations of T-intersections with dead-end fractures demonstrate that density- or pressure-driven flow inside the dead-end branch enhances heat transfer to the rock matrix by sustaining larger temperature differences.
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Stress state, subsidence, and faulting in the Wilmington Oil Field, California: a multiphase flow-geomechanics modeling assessment (1936-2020)
A calibrated multiphase flow-geomechanics model of the Wilmington Oil Field from 1936-2020 indicates that initializing the sedimentary section with low deviatoric stress provides the best fit to historical ground deformation data and implies a shift from the previously assumed reverse-faulting regim