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首页> 外文期刊>International Journal of Heat and Mass Transfer >On a transitional and turbulent natural convection in spherical shells
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On a transitional and turbulent natural convection in spherical shells

机译:关于球形壳中的过渡湍流自然对流

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摘要

Laminar and turbulent natural convection inside concentric spherical shells with isothermal cold and hot boundaries is numerically investigated up to Rayleigh number values Ra ≤ 10~(12) and Pr = 0.71. The study utilizes direct numerical simulation (DNS), large eddy simulation (LES) and Reynolds averaged Navier-Stokes (RANS) approaches for investigation of the laminar, transitional and fully developed turbulent flow regimes, respectively. Three-dimensional flow patterns for slightly supercritical oscillatory flow regime inside the shell, with internal/external diameter ratio equal to D_i/D_o=0.714 are presented and may be potentially useful for verification of the future linear stability analysis results. Particular attention has been given to the complex, fully three-dimensional unsteady flows occurring in narrow shell geometries characterized by 0.85 ≤ D_i/D_o ≤ 0.95. For this geometry considerable deviations in predicted heat flux rate through the shell boundaries are observed when compared with existing heat transfer correlations for the entire range of Ra numbers. The deviations tend to increase for transitional and fully turbulent flows. A new correlation for the heat transfer rate is suggested for laminar and transitional flow regimes.
机译:对具有等温冷热边界的同心球形壳内部的层流和湍流自然对流进行了数值研究,直到瑞利数值Ra≤10〜(12)和Pr = 0.71。这项研究分别利用直接数值模拟(DNS),大涡模拟(LES)和雷诺平均Navier-Stokes(RANS)方法研究层流,过渡和充分发展的湍流状态。提出了壳内部稍超临界振荡流态的三维流型,其内/外直径比等于D_i / D_o = 0.714,可能对验证未来的线性稳定性分析结果有用。特别关注在特征为0.85≤D_i / D_o≤0.95的窄壳几何体中发生的复杂的,全三维非定常流动。对于这种几何形状,当与整个Ra数范围内的现有传热相关性进行比较时,可以观察到通过壳边界的预计热通量有相当大的偏差。对于过渡和完全湍流,偏差趋于增加。对于层流和过渡流动状态,建议了一种新的传热速率相关性。

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