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contributor authorMiressa Ebisa Fola
contributor authorColin D. Rennie
date accessioned2017-05-08T21:50:45Z
date available2017-05-08T21:50:45Z
date copyrightAugust 2010
date issued2010
identifier other%28asce%29hy%2E1943-7900%2E0000222.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/64026
description abstractEmpirical downstream hydraulic geometry equations for consolidated clay-dominated cohesive bed (nonalluvial) natural streams are presented using data from six rivers in eastern Ontario, Canada and four rivers from other regions. The width exponent (0.57) was comparable to the exponents reported for previous studies; however, the depth exponent (0.52) was greater for clay-dominated cohesive bed than for typical alluvial gravel-bed and sand-bed rivers. The width to depth ratio of smaller channels
publisherAmerican Society of Civil Engineers
titleDownstream Hydraulic Geometry of Clay-Dominated Cohesive Bed Rivers
typeJournal Paper
journal volume136
journal issue8
journal titleJournal of Hydraulic Engineering
identifier doi10.1061/(ASCE)HY.1943-7900.0000199
treeJournal of Hydraulic Engineering:;2010:;Volume ( 136 ):;issue: 008
contenttypeFulltext


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