Pulse pressure loading and erosion pattern of cavitating jet

Various erosion patterns generated through the cavitating water jet impacts under ambient pressure conditions were investigated in experiments and numerical simulations. A series of normalized stand-off distances $l_s/d_o $ ∈ [2.5 13.5] were studied during the erosion acceleration period. Two ring-l...

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Main Authors: B. Liu, Y. Pan, F. Ma
Format: Article
Language:English
Published: Taylor & Francis Group 2020-01-01
Series:Engineering Applications of Computational Fluid Mechanics
Subjects:
Online Access:http://dx.doi.org/10.1080/19942060.2019.1695675
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spelling doaj-091d42e74d154600af4670482287804c2020-12-07T17:17:44ZengTaylor & Francis GroupEngineering Applications of Computational Fluid Mechanics1994-20601997-003X2020-01-0114113615010.1080/19942060.2019.16956751695675Pulse pressure loading and erosion pattern of cavitating jetB. Liu0Y. Pan1F. Ma2School of Mechanical Engineering, University of Science and Technology BeijingSchool of Mechanical Engineering, University of Science and Technology BeijingSchool of Mechanical Engineering, University of Science and Technology BeijingVarious erosion patterns generated through the cavitating water jet impacts under ambient pressure conditions were investigated in experiments and numerical simulations. A series of normalized stand-off distances $l_s/d_o $ ∈ [2.5 13.5] were studied during the erosion acceleration period. Two ring-like erosion areas were observed for comparatively low $l_s/d_o $ ∈ [2.5 6.5]. To gain insight into the pulse pressure loading on the erosion area, numerical calculations were performed using the volume of fluid (VOF) interface capturing methodology combined with the large-eddy simulation turbulence model. The erosion patterns are clarified based on the mass loss and distribution features of the eroded regions. The first ring, generated by the cavitation clouds impingement outside the central stagnation area, mainly contributes to the mass loss. The second ring moves inward, merges into the inner ring and eventually vanishes with increasing $l_s/d_o $. High pressure pulsation is found around the locations of the maximum erosion and the approximate intermediate radius of the second ring. The pressure pulsation in the first ring area are dominated by the frequency of the vortices shedding from the jet nozzle. Several higher frequencies are found as the spectral features of the eroded regions in each pattern.http://dx.doi.org/10.1080/19942060.2019.1695675cavitating jetpulse pressurelarge eddy simulationerosion pattern
collection DOAJ
language English
format Article
sources DOAJ
author B. Liu
Y. Pan
F. Ma
spellingShingle B. Liu
Y. Pan
F. Ma
Pulse pressure loading and erosion pattern of cavitating jet
Engineering Applications of Computational Fluid Mechanics
cavitating jet
pulse pressure
large eddy simulation
erosion pattern
author_facet B. Liu
Y. Pan
F. Ma
author_sort B. Liu
title Pulse pressure loading and erosion pattern of cavitating jet
title_short Pulse pressure loading and erosion pattern of cavitating jet
title_full Pulse pressure loading and erosion pattern of cavitating jet
title_fullStr Pulse pressure loading and erosion pattern of cavitating jet
title_full_unstemmed Pulse pressure loading and erosion pattern of cavitating jet
title_sort pulse pressure loading and erosion pattern of cavitating jet
publisher Taylor & Francis Group
series Engineering Applications of Computational Fluid Mechanics
issn 1994-2060
1997-003X
publishDate 2020-01-01
description Various erosion patterns generated through the cavitating water jet impacts under ambient pressure conditions were investigated in experiments and numerical simulations. A series of normalized stand-off distances $l_s/d_o $ ∈ [2.5 13.5] were studied during the erosion acceleration period. Two ring-like erosion areas were observed for comparatively low $l_s/d_o $ ∈ [2.5 6.5]. To gain insight into the pulse pressure loading on the erosion area, numerical calculations were performed using the volume of fluid (VOF) interface capturing methodology combined with the large-eddy simulation turbulence model. The erosion patterns are clarified based on the mass loss and distribution features of the eroded regions. The first ring, generated by the cavitation clouds impingement outside the central stagnation area, mainly contributes to the mass loss. The second ring moves inward, merges into the inner ring and eventually vanishes with increasing $l_s/d_o $. High pressure pulsation is found around the locations of the maximum erosion and the approximate intermediate radius of the second ring. The pressure pulsation in the first ring area are dominated by the frequency of the vortices shedding from the jet nozzle. Several higher frequencies are found as the spectral features of the eroded regions in each pattern.
topic cavitating jet
pulse pressure
large eddy simulation
erosion pattern
url http://dx.doi.org/10.1080/19942060.2019.1695675
work_keys_str_mv AT bliu pulsepressureloadinganderosionpatternofcavitatingjet
AT ypan pulsepressureloadinganderosionpatternofcavitatingjet
AT fma pulsepressureloadinganderosionpatternofcavitatingjet
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