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contributor authorRichard D. Pomeroy
date accessioned2017-05-08T20:38:39Z
date available2017-05-08T20:38:39Z
date copyrightAugust 1983
date issued1983
identifier other%28asce%290733-9429%281983%29109%3A8%281108%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/22158
description abstractMost of the equations that have been developed for relating velocity of a stream in a partly filled pipe to the slope and size of the stream use hydraulic radius (R) as the parameter for Size. The equations using this parameter are poor representations of flow behavior when comparing different relative depths of flow, as Camp pointed out for the case of the Manning equation. If quantity of flow (Q) is used as a parameter for size, an equation is obtained which is very simple to use and which represents flow velocities better than do any of the conventional equations.
publisherAmerican Society of Civil Engineers
titleFlow Velocities in Pipelines
typeJournal Paper
journal volume109
journal issue8
journal titleJournal of Hydraulic Engineering
identifier doi10.1061/(ASCE)0733-9429(1983)109:8(1108)
treeJournal of Hydraulic Engineering:;1983:;Volume ( 109 ):;issue: 008
contenttypeFulltext


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