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dc.contributor.authorDe Simone, Silvia
dc.contributor.authorVilarrasa Riaño, Víctor
dc.contributor.authorCarrera Ramírez, Jesús
dc.contributor.authorAlcolea Rodríguez, Andrés
dc.contributor.authorMeier, Peter
dc.contributor.otherUniversitat Politècnica de Catalunya. Departament d'Enginyeria del Terreny, Cartogràfica i Geofísica
dc.date.accessioned2013-10-11T10:52:25Z
dc.date.created2013-01-17
dc.date.issued2013-01-17
dc.identifier.citationDe Simone, S. [et al.]. Thermal coupling may control mechanical stability of geothermal reservoirs during cold water injection. "Physics and chemistry of the Earth", 17 Gener 2013, vol. 64, p. 1-10.
dc.identifier.issn0079-1946
dc.identifier.urihttp://hdl.handle.net/2117/20363
dc.description.abstractHydraulic stimulation and geothermal reservoir operation may compromise the rock mechanical stability and trigger microseismic events. The mechanisms leading to this induced seismicity are still not completely understood. It is clear that injection causes an overpressure that reduces the effective stress, bringing the system closer to failure conditions. However, rock instability may not result only from hydraulic effects, but also from thermal effects. In fact, hydro-mechanical (i.e., isothermal) models often fail to reproduce field observations because the injection of cold water into a hot reservoir induces thermal stresses due to rock contraction. Thus, rock instability is likely to result from the superposition of hydraulic and thermal effects. Here, we perform coupled thermo-hydro-mechanical and hydro-mechanical simulations to investigate the effects of cold water injection in a fracture zone-intact rock system. Results show that thermal effects induce a significant perturbation on the stress in the intact rock affected by the temperature drop. This perturbation is likely to trigger induced seismicity in the surroundings of critically oriented fractures near the injection well. Hydro-mechanical simulations show that the behavior depends on the orientation of the faults and on the initial stress tensor. In the direction of the fractures, where the strains are more constrained, total stress increases with increasing pressure; thus, deviatoric stress increases or decreases depending on the initial stress state. The comparison between hydraulic and thermal effects shows that, when the largest confining stress acts perpendicular to the fractures, thermoelastic effects dominate and could trigger induced seismicity.
dc.format.extent10 p.
dc.language.isoeng
dc.subjectÀrees temàtiques de la UPC::Enginyeria civil::Geologia::Hidrologia subterrània
dc.subject.lcshInduced seismicity
dc.subject.otherHydraulic stimulation
dc.subject.otherInduced seismicity
dc.subject.otherThermoelasticity
dc.subject.otherElasticity in porous media
dc.subject.otherThermo-hydro-mechanical model
dc.titleThermal coupling may control mechanical stability of geothermal reservoirs during cold water injection
dc.typeArticle
dc.subject.lemacSismicitat inducida
dc.contributor.groupUniversitat Politècnica de Catalunya. GHS - Grup d'Hidrologia Subterrània
dc.identifier.doi10.1016/j.pce.2013.01.001
dc.description.peerreviewedPeer Reviewed
dc.relation.publisherversionhttp://www.sciencedirect.com/science/article/pii/S1474706513000028#
dc.rights.accessRestricted access - publisher's policy
drac.iddocument11807541
dc.description.versionPostprint (published version)
dc.date.lift10000-01-01
upcommons.citation.authorDe Simone, S.; Vilarrasa, V.; Carrera, J.; Alcolea, A.; Meier, P.
upcommons.citation.publishedtrue
upcommons.citation.publicationNamePhysics and chemistry of the Earth
upcommons.citation.volume64
upcommons.citation.startingPage1
upcommons.citation.endingPage10


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