On Steady Two-dimensional Free-surface Flows with Spatially-varied Discharges

In an open-channel, the transition of a flow from a subcritical to a supercritical state may occur as a result of a lateral inflow or outflow that produces a streamwise discharge variation. Apparently, such a transition cannot be modeled accurately by a conventional hydrostatic pressure approach. In...

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Main Author: Zerihun Yebegaeshet T.
Format: Article
Language:English
Published: Sciendo 2019-09-01
Series:Slovak Journal of Civil Engineering
Subjects:
Online Access:http://www.degruyter.com/view/j/sjce.2019.27.issue-3/sjce-2019-0016/sjce-2019-0016.xml?format=INT
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spelling doaj-134c868156204dc1a8b1f09eee4e4a792020-11-25T02:12:50ZengSciendoSlovak Journal of Civil Engineering1338-39732019-09-0127311110.2478/sjce-2019-0016sjce-2019-0016On Steady Two-dimensional Free-surface Flows with Spatially-varied DischargesZerihun Yebegaeshet T.0David & James – Engineering and Environmental Consultancy, Victoria, AustraliaIn an open-channel, the transition of a flow from a subcritical to a supercritical state may occur as a result of a lateral inflow or outflow that produces a streamwise discharge variation. Apparently, such a transition cannot be modeled accurately by a conventional hydrostatic pressure approach. In this study, a depth-averaged model that accounts for the effects of a spatially-varied discharge and a non-hydrostatic pressure distribution was developed and applied to simulate the transcritical flow in a lateral-spillway channel and the subcritical flow in a main channel fitted with side weirs. The model results for the axial free-surface profile and variation of discharge in the main channel were compared with the results of a shallow-flow model and experimental data, thereby resulting in a closer match to the measurements than the shallow-flow model. Overall, the investigation results confirmed the efficiency and validity of the non-hydrostatic depth-averaged model in simulating the mean flow characteristics of the subcritical and transcritical free-surface flows with spatially increasing or decreasing discharges, thus demonstrating its potential to be used as a numerical tool in engineering practice.http://www.degruyter.com/view/j/sjce.2019.27.issue-3/sjce-2019-0016/sjce-2019-0016.xml?format=INThydraulicstructuresside-weir overflownon-hydrostatic flowspatially-varied flownumerical modelside-channel spillway
collection DOAJ
language English
format Article
sources DOAJ
author Zerihun Yebegaeshet T.
spellingShingle Zerihun Yebegaeshet T.
On Steady Two-dimensional Free-surface Flows with Spatially-varied Discharges
Slovak Journal of Civil Engineering
hydraulicstructures
side-weir overflow
non-hydrostatic flow
spatially-varied flow
numerical model
side-channel spillway
author_facet Zerihun Yebegaeshet T.
author_sort Zerihun Yebegaeshet T.
title On Steady Two-dimensional Free-surface Flows with Spatially-varied Discharges
title_short On Steady Two-dimensional Free-surface Flows with Spatially-varied Discharges
title_full On Steady Two-dimensional Free-surface Flows with Spatially-varied Discharges
title_fullStr On Steady Two-dimensional Free-surface Flows with Spatially-varied Discharges
title_full_unstemmed On Steady Two-dimensional Free-surface Flows with Spatially-varied Discharges
title_sort on steady two-dimensional free-surface flows with spatially-varied discharges
publisher Sciendo
series Slovak Journal of Civil Engineering
issn 1338-3973
publishDate 2019-09-01
description In an open-channel, the transition of a flow from a subcritical to a supercritical state may occur as a result of a lateral inflow or outflow that produces a streamwise discharge variation. Apparently, such a transition cannot be modeled accurately by a conventional hydrostatic pressure approach. In this study, a depth-averaged model that accounts for the effects of a spatially-varied discharge and a non-hydrostatic pressure distribution was developed and applied to simulate the transcritical flow in a lateral-spillway channel and the subcritical flow in a main channel fitted with side weirs. The model results for the axial free-surface profile and variation of discharge in the main channel were compared with the results of a shallow-flow model and experimental data, thereby resulting in a closer match to the measurements than the shallow-flow model. Overall, the investigation results confirmed the efficiency and validity of the non-hydrostatic depth-averaged model in simulating the mean flow characteristics of the subcritical and transcritical free-surface flows with spatially increasing or decreasing discharges, thus demonstrating its potential to be used as a numerical tool in engineering practice.
topic hydraulicstructures
side-weir overflow
non-hydrostatic flow
spatially-varied flow
numerical model
side-channel spillway
url http://www.degruyter.com/view/j/sjce.2019.27.issue-3/sjce-2019-0016/sjce-2019-0016.xml?format=INT
work_keys_str_mv AT zerihunyebegaeshett onsteadytwodimensionalfreesurfaceflowswithspatiallyvarieddischarges
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