Please use this identifier to cite or link to this item: http://ir.mu.ac.ke:8080/jspui/handle/123456789/5040
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dc.contributor.authorWahome, John-
dc.contributor.authorBitok, J. K.-
dc.contributor.authorLonyangapuo, J. K.-
dc.contributor.authorKweyu, Cleophas-
dc.contributor.authorNyamai, Benjamin-
dc.date.accessioned2021-08-18T07:46:22Z-
dc.date.available2021-08-18T07:46:22Z-
dc.date.issued2015-
dc.identifier.urihttp://ir.mu.ac.ke:8080/jspui/handle/123456789/5040-
dc.description.abstractDuring heavy rains, open channels are prone to being overrun with storm water. Since the velocity of a flowing fluid increases with depth, sudden overflows may cause velocities to exceed certain limits. This damages the channel by scouring. On the other hand, siltation of suspended matter occurs in sluggish flow. Channel dimensions anden_US
dc.language.isoenen_US
dc.publisherPushpa Publishing Houseen_US
dc.subjectdischargeen_US
dc.subjectwetted perimeteren_US
dc.subjecthydraulic radiusen_US
dc.subjectManning equationen_US
dc.subjectChézy equationen_US
dc.subjectchannel slopeen_US
dc.titleUsing mathematical efficiency criterion to optimize a triangular open channel for stable velocityen_US
dc.typeArticleen_US
Appears in Collections:School of Biological and Physical Sciences

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