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The dissimilarity between spacial and velocity-weighted concentrations

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dc.contributor.authorGuy, Harold P., author
dc.contributor.authorSimons, Daryl B., author
dc.contributor.authorColorado State University, publisher
dc.date.accessioned2019-09-17T18:50:35Z
dc.date.available2019-09-17T18:50:35Z
dc.date.issued1963-01
dc.descriptionCER63HPG-DBS23.
dc.descriptionJanuary 1963.
dc.descriptionAt head of title: United States Department of the Interior Geological Survey.
dc.descriptionIncludes bibliographical references.
dc.description.abstractTheoretical and measured differences between spacial and velocity-weighted concentrations show that (1) the spacial concentration is normally the greater and increases as the velocity and concentration gradients increase, (2) that velocity-weighted concentration must be used to compute sediment discharge, and (3) that spacial concentration must be used to compute the pressure or specific weight on the bed.
dc.format.mediumtechnical reports
dc.identifier.urihttps://hdl.handle.net/10217/197981
dc.languageEnglish
dc.language.isoeng
dc.publisherColorado State University. Libraries
dc.relationCatalog record number (MMS ID): 991013026059703361
dc.relation.ispartofCivil Engineering Reports
dc.relation.ispartofCER, 63-23
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.subjectSedimentation and deposition
dc.subjectSediment transport
dc.subjectBed load -- Measurement
dc.subjectFluid dynamic measurements
dc.titleThe dissimilarity between spacial and velocity-weighted concentrations
dc.title.alternativeDissimilarity between spatial and velocity weighted concentrations
dc.typeText
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