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Examination of Forchheimer equation for crest subsidence, as applied to prismatic channels reveals great dependence of flood wave classification on magnitude of bed slope; it is shown that flood crest will subside and rate of subsidence increases with channel storage available for given depth, and reduces as certain exponent in resistance formula increases; critical examination of discharge in unsteady flow produces improved equations.
Examination of Forchheimer equation for crest subsidence, as applied to prismatic channels reveals great dependence of flood wave classification on magnitude of bed slope; it is shown that flood crest will subside and rate of subsidence increases with channel storage available for given depth, and reduces as certain exponent in resistance formula increases; critical examination of discharge in unsteady flow produces improved equations.
Flood waves in prismatic channels
ASCE -- Proc (J Hydraulics Div)
Henderson, F.M. (author)
1963
29 pages
Article (Journal)
English
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