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dc.contributor.authorLiu, Ko-Feien
dc.contributor.authorWei, Shih-Chaoen
dc.date.accessioned2014-01-30T06:14:21Z-
dc.date.available2014-01-30T06:14:21Z-
dc.date.issued2012-10-08-
dc.identifier.urihttp://hdl.handle.net/2433/180400-
dc.descriptionThe Tenth International Symposium on Mitigation of Geo-disasters in Asia Matsue Symposium Place: Shimane Civil Center, Matsue Date: 8 October 2012en
dc.description.abstractMudflow is a common phenomenon in mountainous area. A lot of researches had simulated debris flows with mudflow. However, either numerical analysis or approximate solutions needs a fundamental solution to work with. In the present paper, we focused on the analytical solutions of fluid mud by using the Bingham fluid model. By using the fact that boundary layer is thin, the solutions of steady uniform flow can be constructed on an inclined rectangular channel. The results can be expressed as function of depth ratio between shear layer to whole layer and Bingham number. The limiting cases for narrow channel and wide one can be discussed by changing the depth width ratio. The solutions on wide channel are the same as other research.en
dc.format.mimetypeapplication/pdf-
dc.language.isoeng-
dc.titleSolutions of laminar mud flow on rectangular channelen
dc.typeconference object-
dc.type.niitypePresentation-
dc.identifier.jtitleMatsue Conference Proceedings (The Tenth International Symposium on Mitigation of Geo-disasters in Asiaen
dc.identifier.spage160-
dc.identifier.epage168-
dc.textversionpublisher-
dc.identifier.artnum共同研究(一般研究集会)24K-02-
dc.sortkey27-
dc.addressDept. of Civil Engineering, National Taiwan University, Taiwan R.O.Cen
dc.addressDept. of Civil Engineering, National Taiwan University, Taiwan R.O.Cen
dcterms.accessRightsopen access-
dc.identifier.jtitle-alternative第10回地震・地盤災害軽減に関するアジア会議及び現地討論会)ja
出現コレクション:Matsue Conference Proceedings

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