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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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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1724908032050069504 |