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dc.contributor.authorZhang, Dawang
dc.contributor.authorCampbell, James
dc.contributor.authorEriksen, Jon Alm
dc.contributor.authorFlekkøy, Eirik Grude
dc.contributor.authorMåløy, Knut Jørgen
dc.contributor.authorMacMinn, Christopher W.
dc.contributor.authorSandnes, Bjørnar
dc.date.accessioned2023-11-13T13:45:08Z
dc.date.available2023-11-13T13:45:08Z
dc.date.created2023-06-09T14:49:49Z
dc.date.issued2023
dc.identifier.citationNature Communications. 2023, 14 (1), .en_US
dc.identifier.issn2041-1723
dc.identifier.urihttps://hdl.handle.net/11250/3102222
dc.description.abstractMultiphase flows involving granular materials are complex and prone to pattern formation caused by competing mechanical and hydrodynamic interactions. Here we study the interplay between granular bulldozing and the stabilising effect of viscous pressure gradients in the invading fluid. Injection of aqueous solutions into layers of dry, hydrophobic grains represent a viscously stable scenario where we observe a transition from growth of a single frictional finger to simultaneous growth of multiple fingers as viscous forces are increased. The pattern is made more compact by the internal viscous pressure gradient, ultimately resulting in a fully stabilised front of frictional fingers advancing as a radial spoke pattern.en_US
dc.language.isoengen_US
dc.publisherNatureen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleFrictional fluid instabilities shaped by viscous forcesen_US
dc.title.alternativeFrictional fluid instabilities shaped by viscous forcesen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.source.pagenumber0en_US
dc.source.volume14en_US
dc.source.journalNature Communicationsen_US
dc.source.issue1en_US
dc.identifier.doi10.1038/s41467-023-38648-6
dc.identifier.cristin2153359
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2


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