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Scalings for unsteady natural convection boundary layers on an evenly heated plate with time-dependent heating flux

机译:时间均匀的热通量在均匀加热板上不稳定自然对流边界层的缩放比例

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摘要

It is of fundamental significance, especially with regard to application, to fully understand the flow behaviornof unsteady natural convection boundary layers on a vertical plate heated by a time-dependent heat flux. Suchnan understanding is currently scarce. In this paper, the scaling analysis by Lin et al. [Phys. Rev. E 79, 066313n(2009)] using a simple three-region structure for the unsteady natural convection boundary layer of a homogeneousnNewtonian fluid with Pr > 1 under isothermal heating was substantially extended for the case when the heating isndue to a time-varying sinusoidal heat flux. A series of scalings was developed for the thermal boundary thickness,nthe plate temperature, the viscous boundary thicknesses, and the maximum vertical velocity within the boundarynlayer, which are the major parameters representing the flow behavior, in terms of the governing parametersnof the flow, i.e., the Rayleigh number Ra, the Prandtl number Pr, and the dimensionless natural frequency fnnof the time-varying sinusoidal heat flux, at the start-up stage, at the transition time scale which represents thenending of the start-up stage and the beginning of the transitional stage of the boundary-layer development, andnat the quasi-steady stage. These scalings were validated by comparison to 10 full numerical solutions of thengoverning equations with Ra, Pr, and fn in the ranges 106 u0002 Ra u0002 109, 3 u0002 Pr u0002 100, and 0.01 u0002 fn u0002 0.1 andnwere shown in general to provide an accurate description of the flow at different development stages, except fornhigh-Pr runs in which a further, although weak, Pr dependence is present, which cannot be accurately predictednby the current scaling analysis using the simple three-region structure, attributed to the non-boundary-layer naturenof the velocity field with high-Pr fluids. Some scalings at the transition time scale and at the quasi-steady stagenalso produce noticeable deviations from the numerical results when fn is reduced, indicating that there may be anfurther fn dependence of the scalings which also cannot be accurately predicted by the current scaling analysis.
机译:尤其是在应用方面,充分理解由时变热流加热的垂直平板上非稳态自然对流边界层的流动行为具有根本的意义。目前对这样的理解尚缺乏。在本文中,由Lin等人进行的尺度分析。 [物理[E. Rev. E 79,066313n(2009)]使用简单的三区域结构,对等温加热下Pr> 1的均质牛顿流体的非稳态自然对流边界层进行了扩展,适用于加热是随时间变化的情况正弦热通量。针对热边界厚度,板温度,粘性边界厚度和边界层内的最大垂直速度,开发了一系列缩放比例,这是代表流动行为的主要参数,代表着流动的控制参数,即,瑞利数Ra,普朗特数Pr和随时间变化的正弦热通量的无量纲固有频率fnn,在启动阶段,过渡时间标度上,代表了启动阶段的结束和边界层发展的过渡阶段和准稳定阶段。通过与Ra,Pr和fn在106 u0002 Ra u0002 109、3 u0002 Pr u0002 100和0.01 u0002 fn u0002范围内的10,n和n的颠倒方程的10个完整数值解进行比较,验证了这些换算。描述不同发展阶段的流量,但高Pr运行除外,尽管存在较高的Pr依赖关系,尽管存在微弱的Pr依赖关系,但当前的比例分析无法使用简单的三区域结构准确地预测到Pr依赖关系,这归因于无边界高P流体的速度场的二层性质。当减小fn时,过渡时间尺度和准稳态阶段的某些比例也会与数值结果产生明显的偏差,这表明可能存在对fn的进一步依赖,这也无法通过当前的比例分析准确地预测。

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  • 来源
    《PHYSICAL REVIEW E》 |2013年第6期|1-17|共17页
  • 作者

    Wenxian Lin; S. W. Armfield;

  • 作者单位

    Solar Energy Research Institute Yunnan Normal University Kunming Yunnan 650092 People’s Republic of ChinaSchool of Engineering James Cook University Townsville QLD 4811 Australia;

    School of Aerospace Mechanical and Mechatronic Engineering University of Sydney NSW 2006 Australia;

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