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dc.date.accessioned2019-05-28T08:37:54Z
dc.date.available2019-05-28T08:37:54Z
dc.date.created2019-01-04T12:22:39Z
dc.date.issued2018
dc.identifier.citationTurquet, Antoine Léo Toussaint, Renaud Eriksen, Fredrik Kvalheim Daniel, Guillaume Koehn, Daniel Flekkøy, Eirik Grude . Microseismic Emissions During Pneumatic Fracturing: A Numerical Model to Explain the Experiments. Journal of Geophysical Research - Solid Earth. 2018, 123(8), 6922-6939
dc.identifier.urihttp://hdl.handle.net/10852/68011
dc.description.abstractModeling of fluid injection processes into a deformable porous medium is a challenging area of physics that has a wide range of applications like the food, construction, and petroleum industries. In this research, we investigate pneumatic fracturing of a porous medium experimentally and numerically in a Hele‐Shaw cell. In the experiments, we inject air into the porous medium (initially random loose packed) to create compaction, channeling, and fracturing while monitoring the cell with accelerometers and a high‐speed camera. Furthermore, we develop a numerical model in two steps: (1) a poroelastoplasticity‐based model to explain dynamic fluid pressure variations and (2) a solid stress model based on Janssen's theory. The contributions of the different pressure sources air in channels and solid stress in the experiments, and the simulations are compared with respect to amplitude and frequency. Afterward, the variations of the normal stress exerting on the plates are convolved with a Lamb Wave green function to generate acoustic emissions numerically. The physics behind the evolution of the experimentally recorded power spectrum of the out‐of‐plane plate vibrations are explained using numerical models. The frequency bands (in the simulated power spectra) are influenced by the size of the opened channels and the Hele‐Shaw cell and are in the same range with the experimentally measured peaks of the acoustic emissions.en_US
dc.languageEN
dc.publisherAmerican Geopgysical Union (AGU)
dc.titleMicroseismic Emissions During Pneumatic Fracturing: A Numerical Model to Explain the Experimentsen_US
dc.typeJournal articleen_US
dc.creator.authorTurquet, Antoine Léo
dc.creator.authorToussaint, Renaud
dc.creator.authorEriksen, Fredrik Kvalheim
dc.creator.authorDaniel, Guillaume
dc.creator.authorKoehn, Daniel
dc.creator.authorFlekkøy, Eirik Grude
cristin.unitcode185,15,4,98
cristin.unitnamePorous Media Laboratory SFF
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2
dc.identifier.cristin1650354
dc.identifier.bibliographiccitationinfo:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Journal of Geophysical Research - Solid Earth&rft.volume=123&rft.spage=6922&rft.date=2018
dc.identifier.jtitleJournal of Geophysical Research - Solid Earth
dc.identifier.volume123
dc.identifier.issue8
dc.identifier.startpage6922
dc.identifier.endpage6939
dc.identifier.doihttp://dx.doi.org/10.1029/2017JB014613
dc.identifier.urnURN:NBN:no-71173
dc.type.documentTidsskriftartikkelen_US
dc.type.peerreviewedPeer reviewed
dc.source.issn2169-9313
dc.identifier.fulltextFulltext https://www.duo.uio.no/bitstream/handle/10852/68011/1/Turquet_et_al-2018-Journal_of_Geophysical_Research__Solid_Earth.pdf
dc.type.versionPublishedVersion


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