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Fluid-to-fluid scaling for convective heat transfer in tubes at supercritical and high subcritical pressures

机译:流体到流体的结垢,在超临界和高亚临界压力下在管道中进行对流换热

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Following a review of two recent sets of fluid-to-fluid scaling laws for supercritical heat transfer and a discussion of their possible limitations, we have proposed two additional sets of scaling laws, which take into account empirically adjustable versions of the Dittus-Boelter correlation and which are applicable to both the supercritical and the high subcritical flow regions. We have compiled a database of heat transfer measurements in carbon dioxide flowing upwards in vertical heated tubes that are free of deterioration or enhancement. We then applied the four sets of scaling laws to these data to compute values of the water-equivalent heat transfer coefficient and compared these values to predictions of a transcritical look-up table, which was earlier shown to represent well a large compilation of measurements in water at supercritical and high subcritical pressures. It was shown that the two earlier methods systematically overestimated the heat transfer coefficient in water and also introduced significant imprecision. In contrast, the two proposed methods of scaling introduce no bias and have lower precision uncertainties than those of the previous scaling methods.
机译:在回顾了两套有关超临界传热的流体-流体比例定律后,并讨论了它们可能的局限性之后,我们提出了另外两套比例定律,其中考虑了Dittus-Boelter相关性的经验可调整形式并且适用于超临界和高亚临界流动区域。我们已经建立了一个在垂直加热管中向上流动的二氧化碳传热测量数据的数据库,该加热管没有劣化或增强。然后,我们将四组缩放定律应用于这些数据,以计算水当量传热系数的值,并将这些值与跨临界查找表的预测进行比较,该跨临界查找表较早地表示可以很好地代表测量的大量汇编。超临界和高亚临界压力下的水。结果表明,两种较早的方法系统地高估了水中的传热系数,并且还引入了明显的不精确性。相反,与先前的缩放方法相比,所提出的两种缩放方法均不引入偏差并且具有较低的精度不确定性。

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