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Computational Analysis of Fluid Dynamics and Heat Transfer Characteristics of a Vibrating Heated Plate

机译:振动加热板流体动力学和传热特性的计算分析

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The introduction of vibrations to a horizontal plate can induce turbulence in the flow field adjacent to the plate under certain combinations of amplitudes and frequency. It is also known that beyond a threshold level of heating, the convective flow field over a heated plate will transition to turbulence. The characterization of the flow field with turbulence in the domain is of paramount importance to ensure a realistic simulation of the flow physics. In the present study, a computational analysis is carried out to characterize the flow regime over a transversely vibrating flat plate (unheated and heated) into laminar or turbulent. The range of frequency and amplitudes of vibrations considered for this analysis are 0 – 150 Hz and 0 – 2 mm respectively. Three different models viz. laminar; Reynolds Averaged Navier-Stokes (RANS) approach with k-ω SST model; and Large-Eddy Simulations (LES) approach with dynamic Smagorinsky-Lilly model are employed, and the results of local, time and space averaged wall shear stress, and the Nusselt number are compared. It has been found that under conditions with unheated or heated vibrating plate, the wall shear stress predictions by all three models are in good agreement with each other with a maximum deviation of 9.5 %. However, when the predictions of local Nusselt number on the heated vibrating plate are compared, it is found that the laminar and LES predictions are in good agreement with each other; the k-ω SST model predictions deviate significantly from the other two models.
机译:在幅度和频率的某些组合下,将振动与水平板的振动引入水平板中的流场中的湍流。还已知超出了加热的阈值水平,加热板上的对流流场将转变为湍流。域中湍流的流场的表征是至关重要的,以确保流量物理学的逼真模拟。在本研究中,进行计算分析,以表征在层流或湍流中的横向振动平板(未加热和加热)上的流动状态。考虑该分析的振动范围和振动的幅度分别为0-150Hz和0-2mm。三种不同的型号viz。层; Reynolds vier-stokes(rans)方法与k-ωsst模型平均;采用了具有动态Smagorinsky-Lilly模型的大涡模拟(LES)方法,并进行了局部,时间和空间平均墙剪应力的结果和纽带数。已经发现,在与未加热或加热的振动板的条件下,所有三种模型的壁剪切应力预测与彼此吻合良好,最大偏差为9.5%。然而,当比较加热的振动板上的局部露珠数的预测时,发现层流和LES预测彼此吻合良好; K-ΩSST模型预测从其他两种模型显着偏离。

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