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Characteristics of bed forms and regimes of flow in alluvial channels

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dc.contributor.authorGarde, R. J., author
dc.contributor.authorAlbertson, Maurice L., author
dc.contributor.authorCivil Engineering Section, Colorado State University, publisher
dc.date.accessioned2017-07-18T13:52:03Z
dc.date.available2017-07-18T13:52:03Z
dc.date.issued1959
dc.descriptionCER59RJG9.
dc.descriptionIncludes bibliographical references (page 17).
dc.description.abstractThe characteristics of the bed and the water surface in an alluvial channel are changed by changing the characteristics of the flow, the fluid, and/or the sediment. This paper first reviews the existing literature on the characteristics of bed forms and regimes of flow over an alluvial bed and then it reports the studies made by the writers about the scale of ripples and dunes and about the criteria for the prediction of different regimes of flow in an alluvial channel.
dc.format.mediumreports
dc.identifier.urihttps://hdl.handle.net/10217/182574
dc.languageEnglish
dc.language.isoeng
dc.publisherColorado State University. Libraries
dc.relationCatalog record number (MMS ID): 991012102099703361
dc.relationTA7.C6 CER 59-9
dc.relation.ispartofCivil Engineering Reports
dc.relation.ispartofCER, 59-9
dc.rightsCopyright and other restrictions may apply. User is responsible for compliance with all applicable laws. For information about copyright law, please see https://libguides.colostate.edu/copyright.
dc.subjectAlluvial streams
dc.subjectSediment transport
dc.titleCharacteristics of bed forms and regimes of flow in alluvial channels
dc.typeText
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