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首页> 外文期刊>International Journal of Heat and Fluid Flow >Higher-order and length-scale statistics of velocity and temperature fluctuations in turbulent boundary layer along a heated vertical flat plate
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Higher-order and length-scale statistics of velocity and temperature fluctuations in turbulent boundary layer along a heated vertical flat plate

机译:沿加热垂直平板的湍流边界层中速度和温度波动的高阶和长尺度统计

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摘要

Time-developing direct numerical simulation (DNS) was performed to clarify the higher-order turbulent behaviors in the thermally-driven boundary layers both in air and water along a heated vertical flat plate. The predicted statistics of the heat transfer rates and the higher-order turbulent behaviors such as skew-ness factors, flatness factors and spatial correlation coefficients of the velocity and temperature fluctuations in the natural-convection boundary layer correspond well with those obtained from experiments for space-developing flows. The numerical results reveal that the turbulent structures of the buoyancy driven boundary layers are mainly controlled by the fluid motions in the outer region of the boundary layer, and these large-scale structures are strongly connected with the generation of turbulence in the thermally-driven boundary layers, in accordance with the actual observations for space-developing flows. Moreover, to specify the turbulence structures of the boundary layers, the cross-correlation coefficients and the characteristic length scales are examined for the velocity and thermal fields. Consequently, it is found that with a slight increase in freestream velocity, the cross-correlation coefficient for the Reynolds shear stress and turbulent heat flux increases for opposing flow and decreases for aiding flow, and the integral scales for the velocity and temperature fields become larger for opposing flow and smaller for aiding flow compared with those for the pure natural-convection boundary layer. (C) 2017 Elsevier Inc. All rights reserved.
机译:进行了时间开发的直接数值模拟(DNS),以阐明沿空气加热的垂直平板在空气和水中的热驱动边界层中的高阶湍流行为。自然对流边界层的传热速率和高阶湍流行为(如偏斜度因子,平面度因子以及速度和温度波动的空间相关系数)的预测统计与空间实验得到的数据非常吻合-开发流程。数值结果表明,浮力驱动边界层的湍流结构主要受边界层外部区域的流体运动控制,这些大尺度结构与热驱动边界层中湍流的产生密切相关。层,根据对空间发展流动的实际观察。此外,为了指定边界层的湍流结构,针对速度场和热场检查了互相关系数和特征长度尺度。因此,发现随着自由流速度的稍微增加,雷诺剪切应力和湍流的通量的互相关系数在逆向流动中增大,而在辅助流动中减小,并且速度场和温度场的积分比例变大与纯自然对流边界层相比,用于逆向流动的流量较小,而用于辅助流动的流量较小。 (C)2017 Elsevier Inc.保留所有权利。

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