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contributor authorBelle R. Samaga
contributor authorKittur G. Ranga Raju
contributor authorRamchandra J. Garde
date accessioned2017-05-08T20:39:27Z
date available2017-05-08T20:39:27Z
date copyrightFebruary 1986
date issued1986
identifier other%28asce%290733-9429%281986%29112%3A11%281019%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/22595
description abstractCareful experiments were conducted on alluvial beds of four sediment mixtures having different arithmetic mean diameters and standard deviations. The suspended load transport rates of individual fractions were measured and compared with both Einstein's and Holtroff's methods of calculation of suspended load for individual fractions. These methods were found to be unsatisfactory in the present range of sediment parameters. A relationship is found to exist between the dimensionless shear stress and the suspended transport rate for uniform sediment. To make this relation applicable to nonuniform sediments, a corrective multiplying factor for shear stress is introduced. The dimensionless parameters which govern this correction factor are identified and a relation for the same obtained. In this manner the relation can be applied to individual size portions of a sediment mixture.
publisherAmerican Society of Civil Engineers
titleSuspended Load Transport of Sediment Mixtures
typeJournal Paper
journal volume112
journal issue11
journal titleJournal of Hydraulic Engineering
identifier doi10.1061/(ASCE)0733-9429(1986)112:11(1019)
treeJournal of Hydraulic Engineering:;1986:;Volume ( 112 ):;issue: 011
contenttypeFulltext


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