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Gradually-varied Flow Profiles in Open Channels [electronic resource] : Analytical Solutions by Using Gaussian Hypergeometric Function / by Chyan-Deng Jan.

By: Jan, Chyan-Deng [author.].
Contributor(s): SpringerLink (Online service).
Material type: materialTypeLabelBookSeries: Advances in Geophysical and Environmental Mechanics and Mathematics: Publisher: Berlin, Heidelberg : Springer Berlin Heidelberg : Imprint: Springer, 2014Description: XIV, 188 p. 34 illus., 7 illus. in color. online resource.Content type: text Media type: computer Carrier type: online resourceISBN: 9783642352423.Subject(s): Physics | Mechanics | Physics | Classical Continuum Physics | MechanicsDDC classification: 531 Online resources: Click here to access online In: Springer eBooksSummary: Gradually-varied flow (GVF) is a steady non-uniform flow in an open channel with gradual changes in its water surface elevation. The evaluation of GVF profiles under a specific flow discharge is very important in hydraulic engineering. This book proposes a novel approach to analytically solve the GVF profiles by using the direct integration and Gaussian hypergeometric function. Both normal-depth- and critical-depth-based dimensionless GVF profiles are presented. The novel approach has laid the foundation to compute at one sweep the GVF profiles in a series of sustaining and adverse channels, which may have horizontal slopes sandwiched in between them
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Gradually-varied flow (GVF) is a steady non-uniform flow in an open channel with gradual changes in its water surface elevation. The evaluation of GVF profiles under a specific flow discharge is very important in hydraulic engineering. This book proposes a novel approach to analytically solve the GVF profiles by using the direct integration and Gaussian hypergeometric function. Both normal-depth- and critical-depth-based dimensionless GVF profiles are presented. The novel approach has laid the foundation to compute at one sweep the GVF profiles in a series of sustaining and adverse channels, which may have horizontal slopes sandwiched in between them

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