Application of the wavelet transform in the laminar turbulent transition for a flow in a mixed convection phenomenon
被引:6
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作者:
Abid, C
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机构:
Univ Aix Marseille, Inst Univ Syst Therm Ind, CNRS, UMR 6995, F-13453 Marseille 13, FranceUniv Aix Marseille, Inst Univ Syst Therm Ind, CNRS, UMR 6995, F-13453 Marseille 13, France
Abid, C
[1
]
Moine, CB
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h-index: 0
机构:
Univ Aix Marseille, Inst Univ Syst Therm Ind, CNRS, UMR 6995, F-13453 Marseille 13, FranceUniv Aix Marseille, Inst Univ Syst Therm Ind, CNRS, UMR 6995, F-13453 Marseille 13, France
Moine, CB
[1
]
Papini, F
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h-index: 0
机构:
Univ Aix Marseille, Inst Univ Syst Therm Ind, CNRS, UMR 6995, F-13453 Marseille 13, FranceUniv Aix Marseille, Inst Univ Syst Therm Ind, CNRS, UMR 6995, F-13453 Marseille 13, France
Papini, F
[1
]
机构:
[1] Univ Aix Marseille, Inst Univ Syst Therm Ind, CNRS, UMR 6995, F-13453 Marseille 13, France
来源:
EUROPEAN PHYSICAL JOURNAL B
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2000年
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13卷
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04期
关键词:
D O I:
10.1007/s100510050089
中图分类号:
O469 [凝聚态物理学];
学科分类号:
070205 ;
摘要:
The aim of this paper is to show the effect of secondary flows caused by natural convection on the laminar-turbulent hydrodynamic transition. It is not a question of measuring a critical threshold value of Reynolds number of transition but only to estimate the degree of turbulence in the transition regime, i.e. weak turbulence in the case of superposition (mixed convection) or not (forced convection) of secondary flows on the forced flow. This is possible thanks to the application of the wavelet transform. The calculation of the Holder exponent, associated with the maximum value of the singularity spectrum for two configurations, vertical (forced convection) and horizontal (mixed convection) allows the degree of turbulence to be measured in both cases. The variation of the Holder exponent versus the Reynolds number has enabled it to be shown that the secondary flows stabilise the main flow and stifle the beginnings of the turbulence during the regime of transition to turbulence; these kinds: of results have also been shown in literature. Generally, large-sized secondary flows (for example Dean's flows) stabilise the turbulence. Our work confirms this, through an experiment carried out in identical conditions for mixed convection (horizontal flow) and forced convection (vertical flow).