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Turbulent vertical convection under vertical vibration

Xinqian Guo, Bo-Fu Wang, Jian-Zhao Wu, Kai Leong Chong, Quan Zhou

2022Physics of Fluids33 citationsDOIOpen Access PDF

Abstract

Vertical convection (VC) under the action of vertical vibration in a square cavity has been investigated using direct numerical simulation. The simulations are conducted with Prandtl number Pr fixed at 4.38 and Rayleigh number Ra ranging from 108 to 1010. To examine the influence of vertical vibration, the dimensionless vibration frequency is varied in the range of 0≤ω≤1000 and a small dimensionless amplitude is fixed at a=1.52×10−3. First, for low vibration frequency, trivial results are obtained where flow structures and the scalings of Nu and Re resemble that of the standard VC cases. In contrast, when the vibration frequency ω increases beyond a critical value ω*, a strong shearing effect from vibration leads to abundant eruptions of thermal plumes from sidewalls, and thus a laminar-turbulent transition of the bulk flow. As a result, heat-transport is greatly enhanced and the scaling exponent β of Nu∼Raβ substantially increases in such the vibration-dominated regime. In specific, the scaling relations obtained transit from Nu∼Ra0.25 and Re∼Ra0.37 at ω = 0 in the laminar regime to Nu∼Ra0.42 and Re∼Ra0.52 at ω≳300 in the turbulent regime. Analysis of the mean flow field shows that the vibration thins the thermal boundary layer and enhances the thermal dissipation rate in the bulk region. Furthermore, we found that the trend of Nu and Re can be well described by the vibrational Rayleigh number Ravib. In particular, Nu is insensitive to Ravib for Ravib≤Ravib*, whereas Nu(ω)/Nu(0)∼(Ravib/Ravib*)0.42 for Ravib>Ravib*, where the critical vibrational Rayleigh number exhibits a scaling relation Ravib*∼Ra0.68 obtained from numerical results.

Topics & Concepts

PhysicsLaminar flowPrandtl numberRayleigh numberDimensionless quantityTurbulenceMechanicsScalingConvectionAmplitudeNatural convectionGeometryOpticsMathematicsFluid Dynamics and Turbulent FlowsWind and Air Flow StudiesPlant Water Relations and Carbon Dynamics