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Conference Paper: Roll waves in mud flow

TitleRoll waves in mud flow
Authors
Issue Date1993
Citation
Proceedings - National Conference On Hydraulic Engineering, 1993 pt 2, p. 1598-1603 How to Cite?
AbstractPermanent roll waves on a shallow layer of fluid mud which is modeled as a power-law fluid is studied. Based on long-wave approximation, momentum integral method is applied to derive the averaged continuity and the momentum equations. Linearized instability analysis of a uniform flow is insufficient to suggest a preferred wavelength for the nonlinear roll waves, which are obtained as periodic shocks connected by smooth profiles. Among all wavelengths only those longer than certain threshold correspond to positive energy loss across the shock, suggesting that a roll wave developed spontaneously form infinitesimal disturbances should have the shortest wavelength corresponding to zero dissipation across the shock, though finite dissipation elsewhere. For longer roll waves, no roll wave exist if the uniform flow is linearly stable, when the fluid is slightly non-Newtonian. However when the fluid is highly non-Newtonian, very long roll waves may still exist even if the corresponding uniform flow is stable to infinitesimal disturbances.
Persistent Identifierhttp://hdl.handle.net/10722/158898

 

DC FieldValueLanguage
dc.contributor.authorNg, Chiuonen_US
dc.contributor.authorMei, Chiang Cen_US
dc.date.accessioned2012-08-08T09:04:28Z-
dc.date.available2012-08-08T09:04:28Z-
dc.date.issued1993en_US
dc.identifier.citationProceedings - National Conference On Hydraulic Engineering, 1993 pt 2, p. 1598-1603en_US
dc.identifier.urihttp://hdl.handle.net/10722/158898-
dc.description.abstractPermanent roll waves on a shallow layer of fluid mud which is modeled as a power-law fluid is studied. Based on long-wave approximation, momentum integral method is applied to derive the averaged continuity and the momentum equations. Linearized instability analysis of a uniform flow is insufficient to suggest a preferred wavelength for the nonlinear roll waves, which are obtained as periodic shocks connected by smooth profiles. Among all wavelengths only those longer than certain threshold correspond to positive energy loss across the shock, suggesting that a roll wave developed spontaneously form infinitesimal disturbances should have the shortest wavelength corresponding to zero dissipation across the shock, though finite dissipation elsewhere. For longer roll waves, no roll wave exist if the uniform flow is linearly stable, when the fluid is slightly non-Newtonian. However when the fluid is highly non-Newtonian, very long roll waves may still exist even if the corresponding uniform flow is stable to infinitesimal disturbances.en_US
dc.languageengen_US
dc.relation.ispartofProceedings - National Conference on Hydraulic Engineeringen_US
dc.titleRoll waves in mud flowen_US
dc.typeConference_Paperen_US
dc.identifier.emailNg, Chiuon:cong@hku.hken_US
dc.identifier.authorityNg, Chiuon=rp00224en_US
dc.description.naturelink_to_subscribed_fulltexten_US
dc.identifier.scopuseid_2-s2.0-0027884401en_US
dc.identifier.issuept 2en_US
dc.identifier.spage1598en_US
dc.identifier.epage1603en_US
dc.identifier.scopusauthoridNg, Chiuon=7401705594en_US
dc.identifier.scopusauthoridMei, Chiang C=7103364150en_US

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