Theoretical Stable Hydraulic Section based on the Principle of Least Action

Abstract Despite decades of effort, stable hydraulic geometry for an open channel water flow has hardly been established because of too many unknown variables for too few rational relationships. This article derives the most efficient channel cross section using calculus of variations for the given...

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Main Authors: Noriaki Ohara, Katsu Yamatani
Format: Article
Language:English
Published: Nature Portfolio 2019-05-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-019-44347-4
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author Noriaki Ohara
Katsu Yamatani
author_facet Noriaki Ohara
Katsu Yamatani
author_sort Noriaki Ohara
collection DOAJ
description Abstract Despite decades of effort, stable hydraulic geometry for an open channel water flow has hardly been established because of too many unknown variables for too few rational relationships. This article derives the most efficient channel cross section using calculus of variations for the given flow area at the minimum wetting perimeter length, which is equivalent to the principle of least action. Analysis indicates that water can most efficiently flow in a semi-ellipse section channel with minimum friction and erosion. Anisotropy in channel erodibility was found to be necessary in the natural stable channel characterization because gravitation force and channel bank consolidation cannot be ignored in earth surface material. This channel cross section, based on the principle of least action, may be regarded as the theoretical stable hydraulic section for erodible bed, which was comparable to the observed river cross-sections during high flow periods.
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spelling doaj.art-2f7901234bd74899a657e9914bf129ba2022-12-21T19:25:33ZengNature PortfolioScientific Reports2045-23222019-05-01911610.1038/s41598-019-44347-4Theoretical Stable Hydraulic Section based on the Principle of Least ActionNoriaki Ohara0Katsu Yamatani1Department of Civil and Architectural Engineering, University of WyomingDepartment of Urban Science, Meijo UniversityAbstract Despite decades of effort, stable hydraulic geometry for an open channel water flow has hardly been established because of too many unknown variables for too few rational relationships. This article derives the most efficient channel cross section using calculus of variations for the given flow area at the minimum wetting perimeter length, which is equivalent to the principle of least action. Analysis indicates that water can most efficiently flow in a semi-ellipse section channel with minimum friction and erosion. Anisotropy in channel erodibility was found to be necessary in the natural stable channel characterization because gravitation force and channel bank consolidation cannot be ignored in earth surface material. This channel cross section, based on the principle of least action, may be regarded as the theoretical stable hydraulic section for erodible bed, which was comparable to the observed river cross-sections during high flow periods.https://doi.org/10.1038/s41598-019-44347-4
spellingShingle Noriaki Ohara
Katsu Yamatani
Theoretical Stable Hydraulic Section based on the Principle of Least Action
Scientific Reports
title Theoretical Stable Hydraulic Section based on the Principle of Least Action
title_full Theoretical Stable Hydraulic Section based on the Principle of Least Action
title_fullStr Theoretical Stable Hydraulic Section based on the Principle of Least Action
title_full_unstemmed Theoretical Stable Hydraulic Section based on the Principle of Least Action
title_short Theoretical Stable Hydraulic Section based on the Principle of Least Action
title_sort theoretical stable hydraulic section based on the principle of least action
url https://doi.org/10.1038/s41598-019-44347-4
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AT katsuyamatani theoreticalstablehydraulicsectionbasedontheprincipleofleastaction