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首页> 外文期刊>International Journal of Heat and Mass Transfer >Boundary layer instability of the natural convection flow on a uniformly heated vertical plate
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Boundary layer instability of the natural convection flow on a uniformly heated vertical plate

机译:均匀加热垂直板上自然对流流动的边界层不稳定性

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摘要

Direct numerical simulation is employed to investigate the two-dimensional boundary layer instability of a natural convection flow on a uniformly heated vertical plate submerged in a homogeneous quiescent environment. A Boussinesq fluid with Prandtl numbers of Pr = 0.733 (air) and 6.7 (water), in the local Ray leigh number range 0 ≤ Ra_x ≤ 2.4 × 10~(10), is studied. Controlled low amplitude numerical disturbances introduced into the base flow excite unstable travelling waves, with the resulting waves tracked and ana lyzed as they travel up the boundary layer. The numerical simulation readily reproduced what is pre dicted by the parallel linear stability theory for the two dimensional mode relatively short wave spectrum, but not for some parts of the long wave spectrum. Critical Rayleigh numbers have been obtained separately for both the temperature and velocity signals using the numerical results, and shown to be in good agreement with each other provided the data is renormalized using the boundary layer sca lings of Sparrow and Greg [1]. It has been shown that the disturbance behavior depends on the Prandtl and Rayleigh numbers, the excitation frequency and to a lesser extent the prescribed thermal coupling at the plate.
机译:直接数值模拟用于研究均质静态环境中浸没在均匀加热的垂直板上自然对流流动的二维边界层不稳定性。研究了局部Ray leigh数范围为0≤Ra_x≤2.4×10〜(10)的普朗特数为Pr = 0.733(空气)和6.7(水)的Boussinesq流体。引入基流中的受控低振幅数值扰动会激发不稳定的行波,并在波沿边界层行进时对所得波进行跟踪和分析。数值模拟很容易地再现了平行线性稳定性理论对二维模式的相对短波谱的预测,但对于长波谱的某些部分则没有。使用数值结果已分别获得了温度和速度信号的临界瑞利数,并且如果使用Sparrow和Greg的边界层标度对数据进行了重新归一化,则表明相互之间具有很好的一致性。已经表明,扰动行为取决于普朗特数和瑞利数,激励频率以及在较小程度上规定的板上热耦合。

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