Please use this identifier to cite or link to this item: http://hdl.handle.net/10603/421372
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dc.coverage.spatialCivil Engineering
dc.date.accessioned2022-12-01T11:15:52Z-
dc.date.available2022-12-01T11:15:52Z-
dc.identifier.urihttp://hdl.handle.net/10603/421372-
dc.description.abstractAlluvial channels with sinuosity follow an altered flow behavior contradictory to straight flows The usual sight of a river system consists of bends or loops along its course Pervious channel boundary allows the transfer of water between the surface and sub surface of a river system Extensive use of groundwater causes depletion or lowering of the groundwater table This has led the channel water to seep away and join the water table underneath commonly known as downward seepage or suction...
dc.format.extentNot Available
dc.languageEnglish
dc.relationNot Available
dc.rightsself
dc.titleHydromorphology of sinuous river system with and without downward seepage
dc.title.alternativeNot available
dc.creator.researcherTaye, Jyotismita
dc.subject.keywordEngineering
dc.subject.keywordEngineering and Technology
dc.subject.keywordEngineering Civil
dc.description.noteNot Available
dc.contributor.guideKumar, Bimlesh
dc.publisher.placeGuwahati
dc.publisher.universityIndian Institute of Technology Guwahati
dc.publisher.institutionDEPARTMENT OF CIVIL ENGINEERING
dc.date.registered2017
dc.date.completed2021
dc.date.awarded2021
dc.format.dimensionsNot Available
dc.format.accompanyingmaterialNone
dc.source.universityUniversity
dc.type.degreePh.D.
Appears in Departments:DEPARTMENT OF CIVIL ENGINEERING

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