Formation mechanism of suction vortices in a pump sump

The origin and formation mechanism of a submerged vortex and an air-entraining vortex have been fully clarified by large-eddy simulation (LES) that used approximately 2 billion hexahedral elements with maximum resolution of 0.255 mm and was applied to the internal flows of a model pump sump. The mod...

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Main Authors: Yoshinobu YAMADE, Chisachi KATO, Takahide NAGAHARA, Jun MATSUI
Format: Article
Language:Japanese
Published: The Japan Society of Mechanical Engineers 2019-06-01
Series:Nihon Kikai Gakkai ronbunshu
Subjects:
Online Access:https://www.jstage.jst.go.jp/article/transjsme/85/875/85_19-00072/_pdf/-char/en
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author Yoshinobu YAMADE
Chisachi KATO
Takahide NAGAHARA
Jun MATSUI
author_facet Yoshinobu YAMADE
Chisachi KATO
Takahide NAGAHARA
Jun MATSUI
author_sort Yoshinobu YAMADE
collection DOAJ
description The origin and formation mechanism of a submerged vortex and an air-entraining vortex have been fully clarified by large-eddy simulation (LES) that used approximately 2 billion hexahedral elements with maximum resolution of 0.255 mm and was applied to the internal flows of a model pump sump. The model pump sump is composed of a 2,500 mm-long water channel of rectangular cross section with a width of 300 mm and a water depth of 100 mm and a vertical suction pipe with a 100 mm diameter installed at its downstream end with an offset of 10 mm from the centerline of the rectangular channel. At the upstream end of the channel, a uniform velocity of 0.37 m/s is given. LES with different wall boundary conditions have revealed that the origin of a submerged vortex is the mean shear of the approaching boundary layers that develop on the bottom and side walls of the pump sump. From detailed investigations of LES computed for a long time period of 16 seconds have revealed that deviation of the mean flow that approaches the suction pipe triggers conversion of the axis of the vorticity that was originally aligned to the lateral direction in the approaching boundary layers to that aligned to the vertical direction. The local acceleration of the vertical flow stretches the afore-mentioned vertical vortex, which results in formation of a submerged vortex. The separated flows downstream of the suction pipe generate vertical vorticity, and forms an air-entraining vortex when such a vortex is sucked into the suction pipe. Computations with a different bellmouth height and a different water-surface height have supported the above mentioned origin and formation mechanism of these vortices.
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spelling doaj.art-270e7051c7cc4a44b4ee3c9c04116c382022-12-22T04:16:11ZjpnThe Japan Society of Mechanical EngineersNihon Kikai Gakkai ronbunshu2187-97612019-06-018587519-0007219-0007210.1299/transjsme.19-00072transjsmeFormation mechanism of suction vortices in a pump sumpYoshinobu YAMADE0Chisachi KATO1Takahide NAGAHARA2Jun MATSUI3Mizuho Information & Research Institute, Inc.Institute of Industrial Science, The University of TokyoIndustrial Products Company, Hitachi, Ltd.Faculty of Engineering, Yokohama National UniversityThe origin and formation mechanism of a submerged vortex and an air-entraining vortex have been fully clarified by large-eddy simulation (LES) that used approximately 2 billion hexahedral elements with maximum resolution of 0.255 mm and was applied to the internal flows of a model pump sump. The model pump sump is composed of a 2,500 mm-long water channel of rectangular cross section with a width of 300 mm and a water depth of 100 mm and a vertical suction pipe with a 100 mm diameter installed at its downstream end with an offset of 10 mm from the centerline of the rectangular channel. At the upstream end of the channel, a uniform velocity of 0.37 m/s is given. LES with different wall boundary conditions have revealed that the origin of a submerged vortex is the mean shear of the approaching boundary layers that develop on the bottom and side walls of the pump sump. From detailed investigations of LES computed for a long time period of 16 seconds have revealed that deviation of the mean flow that approaches the suction pipe triggers conversion of the axis of the vorticity that was originally aligned to the lateral direction in the approaching boundary layers to that aligned to the vertical direction. The local acceleration of the vertical flow stretches the afore-mentioned vertical vortex, which results in formation of a submerged vortex. The separated flows downstream of the suction pipe generate vertical vorticity, and forms an air-entraining vortex when such a vortex is sucked into the suction pipe. Computations with a different bellmouth height and a different water-surface height have supported the above mentioned origin and formation mechanism of these vortices.https://www.jstage.jst.go.jp/article/transjsme/85/875/85_19-00072/_pdf/-char/enpump sumpsuction vorticessubmerged vorticesair-entraining vorticieslarge eddy simulationformation mechanism
spellingShingle Yoshinobu YAMADE
Chisachi KATO
Takahide NAGAHARA
Jun MATSUI
Formation mechanism of suction vortices in a pump sump
Nihon Kikai Gakkai ronbunshu
pump sump
suction vortices
submerged vortices
air-entraining vorticies
large eddy simulation
formation mechanism
title Formation mechanism of suction vortices in a pump sump
title_full Formation mechanism of suction vortices in a pump sump
title_fullStr Formation mechanism of suction vortices in a pump sump
title_full_unstemmed Formation mechanism of suction vortices in a pump sump
title_short Formation mechanism of suction vortices in a pump sump
title_sort formation mechanism of suction vortices in a pump sump
topic pump sump
suction vortices
submerged vortices
air-entraining vorticies
large eddy simulation
formation mechanism
url https://www.jstage.jst.go.jp/article/transjsme/85/875/85_19-00072/_pdf/-char/en
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AT takahidenagahara formationmechanismofsuctionvorticesinapumpsump
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