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dc.contributor.authorLien, HCen_US
dc.contributor.authorYeh, KCen_US
dc.contributor.authorYang, JCen_US
dc.date.accessioned2014-12-08T15:27:25Z-
dc.date.available2014-12-08T15:27:25Z-
dc.date.issued1997en_US
dc.identifier.isbn0-7844-0272-8en_US
dc.identifier.urihttp://hdl.handle.net/11536/19687-
dc.description.abstractThe purpose of this paper is to simulate the migration of a pit in the channel bed. When water flows over a pit, the velocity at the upstream end of the pit slows down rapidly owing to the increment of the flow depth, and that at the downstream end of the pit speeds up because of the sudden contraction of the now area. Under such a flow condition, the equilibrium sediment transport formula is inadequate to simulate the local deposition and scouring around the pit. In addition, the critical bed-shear stress without considering the bed slope effect may increase the deposition rate near the upstream end and the scouring rate near the downstream end of the pit. This paper proposes a numerical model to simulate the migration of a pit by considering the nonequilibrium sediment transport behavior and the modified critical bed-shear stress for the movement of sediment on the large bed slope. The capability of the model was verified by comparing the simulated results with one of the experiments executed by Lee et at. (1993).en_US
dc.language.isoen_USen_US
dc.titleNumerical simulation of the pit migrationen_US
dc.typeProceedings Paperen_US
dc.identifier.journalENVIRONMENTAL AND COASTAL HYDRAULICS: PROTECTING THE AQUATIC HABITAT, PROCEEDINGS OF THEME B, VOLS 1 & 2en_US
dc.citation.volume27en_US
dc.citation.spage1185en_US
dc.citation.epage1190en_US
dc.contributor.department土木工程學系zh_TW
dc.contributor.departmentDepartment of Civil Engineeringen_US
dc.identifier.wosnumberWOS:000081412000200-
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