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dc.contributor.authorUcar, Eren
dc.contributor.authorBerre, Inga
dc.contributor.authorKeilegavlen, Eirik
dc.date.accessioned2018-03-14T14:08:55Z
dc.date.available2018-03-14T14:08:55Z
dc.date.issued2017-10-04
dc.identifier.issn1944-8007en_US
dc.identifier.issn0094-8276en_US
dc.identifier.urihttps://hdl.handle.net/1956/17515
dc.description.abstractUnderstanding the controlling mechanisms underlying injection-induced seismicity is important for optimizing reservoir productivity and addressing seismicity-related concerns related to hydraulic stimulation in Enhanced Geothermal Systems. Hydraulic stimulation enhances permeability through elevated pressures, which cause normal deformations and the shear slip of preexisting fractures. Previous experiments indicate that fracture deformation in the normal direction reverses as the pressure decreases, e.g., at the end of stimulation. We hypothesize that this normal closure of fractures enhances pressure propagation away from the injection region and significantly increases the potential for postinjection seismicity. To test this hypothesis, hydraulic stimulation is modeled by numerically coupling flow in the fractures and matrix, fracture deformation, and matrix deformation for a synthetic reservoir in which the flow and mechanics are strongly affected by a complex three-dimensional fracture network. The role of the normal closure of fractures is verified by comparing simulations conducted with and without the normal closure effect.en_US
dc.language.isoengeng
dc.publisherAmerican Geophysical Unionen_US
dc.relation.ispartof<a href="http://hdl.handle.net/1956/17514" target="blank">Numerical modeling of shear stimulation in naturally fractured geothermal reservoirs</a>en_US
dc.titlePostinjection Normal Closure of Fractures as a Mechanism for Induced Seismicityen_US
dc.typePeer reviewed
dc.typeJournal article
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright AGU. All rights reserved.en_US
dc.source.journalGeophysical Research Letters
dc.source.4044
dc.source.1419
dc.source.pagenumber9598-9606
dc.subject.nsiVDP::Matematikk og Naturvitenskap: 400::Matematikk: 410::Anvendt matematikk: 413en_US


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