Origin and formation process of a submerged vortex in a pump sump. Issue 3 (March 2019)

• Record Type: Journal Article
• Authors: Yamade, Y; Kato, C; Nagahara, T; Matsui, Jun
• Is Part Of: IOP conference series. Volume 240:Issue 3(2019)
• Publication Date: 2019-03
• Subjects: Earth sciences -- Periodicals; Environmental sciences -- Congresses; Environmental sciences -- Periodicals; 550.5
• DOI: 10.1088/1755-1315/240/3/032028
• Languages: English
• ISSNs: 1755-1307

Abstract

Abstract: The origin and formation process of a submerged vortex have been fully clarified by large-eddy simulation (LES) that used approximately of 250 million hexahedral elements with maximum resolution of 0.450 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. 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. 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 the formation of a strong submerged vortex. A computation with a different height of the vermouth inlet has supported the above mentioned formation process of a submerged vortex.