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Investigation on the mechanism of abnormal heat transfer of supercritical pressure water in vertically-upward tubes in the large specific heat region

机译:大特定热区垂直向上管中超临界压力异常传热机理的研究

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The heat transfer characteristics of water at supercritical pressures in a vertically-upward internally-ribbed tube are investigated experimentally to investigate the mechanism of abnormal heat transfer of supercritical pressure water in the so-called large specific heat region. One kind optimized internally-ribbed tube is used in this study. The tube is made of SA-213T12 steel with an outer diameter of 31.8 mm and a wall thickness of 6 mm and the mean inside diameter of the tube is measured to be 17.63 mm. According to experimental data, the characteristics and mechanisms of the heat transfer enhancement and also the heat transfer deterioration of supercritical pressure water in the large specific heat region are discussed respectively. The heat transfer enhancement of the supercritical pressure water in the large specific heat region is believed to be a result of combined effect caused by the rapid variations of thermophysical properties of the supercritical pressure water in the large specific heat region, and the same is true of the heat transfer deterioration. The drastic changes in thermophysical properties near the pseudocritical points, especially the sudden rise in the specific heat of water at supercritical pressures, may result in the occurrence of the heat transfer enhancement, while the covering of the heat transfer surface by fluids lighter and hotter than the bulk fluid makes the heat transfer deteriorated eventually and explains how this lighter fluid layer forms. It is also found that the heat transfer deterioration of water at supercritical pressures is similar to the DNB (departure from nucleate boiling) at subcritical pressures in mechanism.
机译:实验研究了垂直向上内肋管中的超临界压力下水的热传递特性,以研究所谓的大特定热区中超临界压力异常传热异常传热的机理。本研究使用了一种优化的内肋管。该管由SA-213T12钢制成,外径为31.8mm,壁厚6mm,测量管的平均内径为17.63mm。根据实验数据,分别讨论了传热增强的特性和机制以及大特定热区中超临界压力的传热劣化。据信,大特定热区域中超临界压力的传热增强是由大特定热区域中超临界压力的快速变化引起的组合效应的结果,并且相同传热劣化。伪关键附近的热物理特性的激烈变化,特别是水在超临界压力下的比水热突然上升,可能导致传热增强的发生,而传热表面的覆盖较轻,比散装流体最终使热传递劣化,并解释了这种较轻的流体层的形式。还发现,在机理中的亚临界压力下,超临界压力下水的热传递劣化类似于亚临界压力的DNB(脱离核心沸腾)。

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