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dc.contributor.authorZhao, Xiaomin
dc.contributor.authorToksoz, M. Nafi
dc.contributor.otherMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.date.accessioned2012-12-04T14:50:04Z
dc.date.available2012-12-04T14:50:04Z
dc.date.issued1992
dc.identifier.urihttp://hdl.handle.net/1721.1/75189
dc.description.abstractA stable Alternating Direction Implicit finite-difference algorithm is used to model transient fluid flow in heterogeneous porous media. In connection with the laboratory system for pressure transient testing of core permeability, the effects of permeability heterogeneities on the characteristics of the pressure transient were investigated. The results show that the early portion of the pressure transient is sensitive to the heterogeneity, while the late time portion is primarily controlled by the effective permeability of the sample. As in the steady flow case, lineation in permeability distribution produces anisotropy in measured permeability. Particularly, in the case of lineated fractures, where the background permeability is small, such anisotropy can produce an order of magnitude difference in permeability.en_US
dc.description.sponsorshipMassachusetts Institute of Technology. Borehole Acoustics and Logging Consortiumen_US
dc.description.sponsorshipUnited States. Dept. of Energy (Grant DE-FG02-86ER13636)en_US
dc.publisherMassachusetts Institute of Technology. Earth Resources Laboratoryen_US
dc.relation.ispartofseriesEarth Resources Laboratory Industry Consortia Annual Report;1992-06
dc.titleTransient Fluid Flow In Heterogeneous Porous Mediaen_US
dc.typeTechnical Reporten_US
dc.contributor.mitauthorZhao, Xiaomin
dc.contributor.mitauthorToksoz, M. Nafi
dspace.orderedauthorsZhao, Xiaomin; Toksoz, M. Nafien_US


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