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Effects of Free Stream Velocity on Turbulent Natural Convection Flow Over a Vertical Forward-Facing Step

机译:自由流速度对垂直前向台阶湍流自然对流的影响

摘要

Measurements of heat transfer and fluid flow of turbulent boundary-layer air flow in natural and mixed convection over an isothermal two-dimensional, vertical forward-facing step are reported. The upstream and downstream walls and the step itself were heated to a uniform and constant temperature. Air velocity and temperature distributions and their turbulent fluctuations are measured simultaneously using a two-component laser-Doppler velocimeter (LDV) and a cold wire anemometer, respectively. The present study treats buoyancy-dominated mixed convection over a vertical forward-facing step and examines the effect of a small free stream velocity on turbulent natural convection. The experiment was carried out for a step height of 22 mm, for a range of free stream air velocities 0 m/s u26leg; u ∞ u26leg; 0.55 m/s (corresponding to a range of Reynolds numbers of 0 u26leg; Rebinf{s} u26leg; 712), and a temperature difference, ΔT, of 30°C between the heated walls and the free stream air (corresponding to a local Grashof number Gr xi = 6.45 × 10 10 ). It was found that the reattachment length increases while the heat transfer rate from the downstream heated wall decreases as the small free stream velocity increases.
机译:报告了在等温二维垂直垂直向前步骤中自然对流和混合对流中边界层湍流的热传递和流体流动的测量结果。将上游和下游壁以及台阶本身加热至均匀且恒定的温度。分别使用两分量激光多普勒测速仪(LDV)和冷线风速仪同时测量风速和温度分布及其湍流波动。本研究在垂直向前的步骤中处理浮力主导的混合对流,并研究了小自由流速度对湍流自然对流的影响。实验是针对22 mm的台阶高度进行的,自由气流速度范围为0 m / s。 u∞ u26leg; 0.55 m / s(对应于0的雷诺数范围; Reabinf {s}的范围; 712),并且加热的壁和自由气流之间的温度差ΔT为30°C(对应于当地的Grashof数Gr xi = 6.45×10 10)。已发现,随着小自由流速度的增加,重新连接长度增加,而来自下游加热壁的传热速率降低。

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