Unsteadiness and Modal Analysis of Ridge Ice-Induced Separation in Post-Stall Conditions via IDDES

High-resolution simulation of shear layer oscillation induced by ridge ice in post-stall condition is conducted via the improved delayed detached-eddy simulation (IDDES) method. The flow-field evolution characteristics of large scale separation in high Reynolds number condition are described. It is...

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Autor principal: TAN Xue, ZHANG Chen, XU Wenhao, WANG Fuxin, WEN Minhua
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Publicado: Editorial Office of Journal of Shanghai Jiao Tong University 2021
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Acceso en línea:https://doaj.org/article/c01bd97e7bc94207843526a6194b8ac2
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spelling oai:doaj.org-article:c01bd97e7bc94207843526a6194b8ac22021-12-03T02:59:23ZUnsteadiness and Modal Analysis of Ridge Ice-Induced Separation in Post-Stall Conditions via IDDES1006-246710.16183/j.cnki.jsjtu.2020.427https://doaj.org/article/c01bd97e7bc94207843526a6194b8ac22021-11-01T00:00:00Zhttp://xuebao.sjtu.edu.cn/article/2021/1006-2467/1006-2467-55-11-1333.shtmlhttps://doaj.org/toc/1006-2467High-resolution simulation of shear layer oscillation induced by ridge ice in post-stall condition is conducted via the improved delayed detached-eddy simulation (IDDES) method. The flow-field evolution characteristics of large scale separation in high Reynolds number condition are described. It is shown that the ridge ice and trailing edge of the lower surface induce the development of shear flow at the same time. The wall is not reattached by the shear layer induced by ridge ice, and the “up-wash” flow from the lower surface is interacted with the shear layer, which lead to the formation of large-scale coherent structures. Combined with the spectral analysis, the pressure pulsation located in the shear layer is characterized by two typical frequencies, which are associated with Kelvin-Helmholtz instability and appear as the vortex pairing and shedding. Based on the proper orthogonal decomposition, the dominant mode of pressure pulsation between shear layers is extracted as large-scale coherent structures. The same peak value is shown in power density spectrum of dominant mode temporal coefficient and lift coefficient, which indicates that the large-scale coherent structure is connected with lift fluctuation.TAN Xue, ZHANG Chen, XU Wenhao, WANG Fuxin, WEN MinhuaEditorial Office of Journal of Shanghai Jiao Tong Universityarticleridge iceshear layer oscillationnumerical simulationspectrum analysismodal analysisEngineering (General). Civil engineering (General)TA1-2040Chemical engineeringTP155-156Naval architecture. Shipbuilding. Marine engineeringVM1-989ZHShanghai Jiaotong Daxue xuebao, Vol 55, Iss 11, Pp 1333-1342 (2021)
institution DOAJ
collection DOAJ
language ZH
topic ridge ice
shear layer oscillation
numerical simulation
spectrum analysis
modal analysis
Engineering (General). Civil engineering (General)
TA1-2040
Chemical engineering
TP155-156
Naval architecture. Shipbuilding. Marine engineering
VM1-989
spellingShingle ridge ice
shear layer oscillation
numerical simulation
spectrum analysis
modal analysis
Engineering (General). Civil engineering (General)
TA1-2040
Chemical engineering
TP155-156
Naval architecture. Shipbuilding. Marine engineering
VM1-989
TAN Xue, ZHANG Chen, XU Wenhao, WANG Fuxin, WEN Minhua
Unsteadiness and Modal Analysis of Ridge Ice-Induced Separation in Post-Stall Conditions via IDDES
description High-resolution simulation of shear layer oscillation induced by ridge ice in post-stall condition is conducted via the improved delayed detached-eddy simulation (IDDES) method. The flow-field evolution characteristics of large scale separation in high Reynolds number condition are described. It is shown that the ridge ice and trailing edge of the lower surface induce the development of shear flow at the same time. The wall is not reattached by the shear layer induced by ridge ice, and the “up-wash” flow from the lower surface is interacted with the shear layer, which lead to the formation of large-scale coherent structures. Combined with the spectral analysis, the pressure pulsation located in the shear layer is characterized by two typical frequencies, which are associated with Kelvin-Helmholtz instability and appear as the vortex pairing and shedding. Based on the proper orthogonal decomposition, the dominant mode of pressure pulsation between shear layers is extracted as large-scale coherent structures. The same peak value is shown in power density spectrum of dominant mode temporal coefficient and lift coefficient, which indicates that the large-scale coherent structure is connected with lift fluctuation.
format article
author TAN Xue, ZHANG Chen, XU Wenhao, WANG Fuxin, WEN Minhua
author_facet TAN Xue, ZHANG Chen, XU Wenhao, WANG Fuxin, WEN Minhua
author_sort TAN Xue, ZHANG Chen, XU Wenhao, WANG Fuxin, WEN Minhua
title Unsteadiness and Modal Analysis of Ridge Ice-Induced Separation in Post-Stall Conditions via IDDES
title_short Unsteadiness and Modal Analysis of Ridge Ice-Induced Separation in Post-Stall Conditions via IDDES
title_full Unsteadiness and Modal Analysis of Ridge Ice-Induced Separation in Post-Stall Conditions via IDDES
title_fullStr Unsteadiness and Modal Analysis of Ridge Ice-Induced Separation in Post-Stall Conditions via IDDES
title_full_unstemmed Unsteadiness and Modal Analysis of Ridge Ice-Induced Separation in Post-Stall Conditions via IDDES
title_sort unsteadiness and modal analysis of ridge ice-induced separation in post-stall conditions via iddes
publisher Editorial Office of Journal of Shanghai Jiao Tong University
publishDate 2021
url https://doaj.org/article/c01bd97e7bc94207843526a6194b8ac2
work_keys_str_mv AT tanxuezhangchenxuwenhaowangfuxinwenminhua unsteadinessandmodalanalysisofridgeiceinducedseparationinpoststallconditionsviaiddes
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