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dc.contributor.authorToksoz, M. Nafi
dc.contributor.authorZhang, Yang
dc.date.accessioned2012-10-04T19:08:38Z
dc.date.available2012-10-04T19:08:38Z
dc.date.issued2012-03
dc.date.submitted2011-11
dc.identifier.issn1070-485X
dc.identifier.issn0016-8033
dc.identifier.urihttp://hdl.handle.net/1721.1/73617
dc.description.abstractWith the current developments in imaging/computational techniques and resources, computational rock physics has been emerging as a new field of study. Properties of rocks are examined by carrying out extensive numerical simulations on rocks that have been digitized using high-resolution X-ray CT scans. The ultimate goal of computational rock physics is to supplement the traditional laboratory measurements, which are time consuming, with faster numerical simulations that allow the parameter space to be explored more thoroughly. We applied the finite-element method to compute the static effective elastic properties from 3D microtomographic images of Berea sandstone saturated with different fluids. From the computations, we found discrepancies between the numerical results and the laboratory measurements. The reason for such a problem is the loss of small features, such as fine cracks and micropores, in the digitized matrix during the imaging and aggregation process. We used a hybrid approach, combining the numerical computation and the effective media theories — the differential effective medium model and the Kuster-Toksöz model — to deduce the lost cracks by a very fast simulated annealing method. We analyzed the sensitivity of the inverted results — the distributions of crack aspect ratios and concentrations — to the clay content. We found that the inverted crack distribution is not so sensitive to clay content. Compared with the effect of cracks on the computed effective elastic properties, clay has only a secondary effect. Our approach can recover the lost cracks and is capable of predicting the effective elastic properties of the rocks from the microtomographic images for different fluid saturations. Compared with the traditional inversion schemes, based only on the effective media theories, this hybrid scheme has the advantage of utilizing the complex microstructures that are resolved in the imaging process, and it helps define the inversion space for crack distribution.en_US
dc.description.sponsorshipSchlumberger-Doll Research Centeren_US
dc.description.sponsorshipMassachusetts Institute of Technology. Earth Resources Laboratory Founding Member Consortiumen_US
dc.description.sponsorshipSaudi Aramco (Fellowship)en_US
dc.language.isoen_US
dc.publisherSociety of Exploration Geophysicistsen_US
dc.relation.isversionofhttp://dx.doi.org/10.1190/geo2011-0126.1en_US
dc.rightsArticle is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use.en_US
dc.sourceSociety of Exploration Geophysicistsen_US
dc.titleImpact of the cracks lost in the imaging process on computing linear elastic properties from 3D microtomographic images of Berea sandstoneen_US
dc.typeArticleen_US
dc.identifier.citationZhang, Yang, and M. Nafi Toksöz. “Impact of the Cracks Lost in the Imaging Process on Computing Linear Elastic Properties from 3D Microtomographic Images of Berea Sandstone.” Geophysics 77.2 (2012): R95. ©2012 Society of Exploration Geophysicistsen_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciencesen_US
dc.contributor.mitauthorToksoz, M. Nafi
dc.contributor.mitauthorZhang, Yang
dc.relation.journalGeophysicsen_US
dc.eprint.versionFinal published versionen_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dspace.orderedauthorsZhang, Yang; Toksöz, M. Nafien
dc.identifier.orcidhttps://orcid.org/0000-0002-4851-3089
mit.licensePUBLISHER_POLICYen_US
mit.metadata.statusComplete


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