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dc.contributor.authorNordhaug, Hans Fredrikeng
dc.contributor.authorCelia, Michael A.eng
dc.contributor.authorDahle, Helge K.eng
dc.date.accessioned2007-04-03T13:22:11Z
dc.date.available2007-04-03T13:22:11Z
dc.date.issued2003eng
dc.PublishedAdvances in Water Resources 2003 26(10):1061-1074en
dc.identifier.urihttps://hdl.handle.net/1956/2201
dc.descriptionThe authors final, peer-reviewed postprint version of the article.
dc.description.abstractTwo-phase flow in porous media is characterized by fluid-fluid interfaces that separate the fluid phases at the pore scale. These interfaces support pressure differences between phases, and their dynamics allow for saturation changes within the porous medium. Dynamic porescale network models allow interface dynamics to be modeled explicitly, such that each fluid-fluid interface within a network of pores is tracked explicitly in space and time. Because these models produce a detailed description of both phase and interface dynamics, results from these models can be averaged to provide values for many upscaled variables. These include nontraditional variables such as amounts of interfacial area, and volumeaveraged interfacial velocities. While these upscaled variables provide insights into the underlying dynamics of two-phase flow systems, they also allow new theories involving interfacial area to be tested directly. Results from a test of one such theory reveals that proposed constitutive equations involving interfacial velocities fail to match results from the network model for most cases considered. Therefore the macroscopic equations require additional development before they can be used for macro-scale simulations.en_US
dc.format.extent2613751 byteseng
dc.format.mimetypeapplication/pdfeng
dc.language.isoengeng
dc.publisherElsevier Scienceen_US
dc.subjectTwo-phase floweng
dc.subjectDynamic pore-scale network modelseng
dc.subjectInterfacial areaeng
dc.subjectUpscalingeng
dc.titleA pore network model for calculation of interfacial velocitiesen_US
dc.typePeer reviewed
dc.typeJournal article
dc.identifier.doihttps://doi.org/10.1016/s0309-1708(03)00100-3
dc.subject.nsiVDP::Matematikk og Naturvitenskap: 400::Matematikk: 410nob


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