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Pressure Drop and Void Fraction in Horizontal Air–Water Stratified Flows with Smooth Interface at Atmospheric Pressure

机译:水平空气分层流量下降和空隙率,具有大气压的光滑界面

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This work presents and analyses the results of an experimental activity aimed at the characterization of stratified air–water flow conditions, which have been poorly analyzed in previous studies although they are significant for industrial applications. Tests were performed in a 24 m long, 60 mm inner diameter PMMA pipe; the superficial velocities ranged between 0.03 m/s and 0.06 m/s for the water and between 0.41 m/s and 2.31 m/s for air. The pressure gradient along the pipeline was determined and compared to the one obtained implementing two-fluid models available in the literature. Fair agreement with the models was found only at high values of the superficial gas velocities, i.e., above 1.31 m/s. Moreover, the void fraction was measured through a resistive probe and compared with the values predicted by available models. Since none of them was able to satisfactorily predict the void fraction in the whole range of superficial velocities, a drift flux model was successfully implemented. Eventually, with both the measured pressure gradient and the void fraction, a two-fluid model was implemented in order to determine the interfacial shear stress and to compare the outcome with the literature, emphasizing the influence of the operating conditions on the prediction performance.
机译:该工作介绍并分析了旨在表征分层空气流动条件的实验活动的结果,这在先前的研究中已经很差,尽管它们对工业应用具有重要意义。测试是在24米长,60毫米内径PMMA管中进行的。表面速度范围为0.03m / s和0.06m / s,水为0.41m / s和2.31米/秒。测定沿管道的压力梯度并与在文献中可用的实施的双流体模型获得的梯度进行比较。与模型的公平协议仅在高于浅表气体速度的高值下发现,即1.31米/秒。此外,通过电阻探针测量空隙部分,并与可用模型预测的值进行比较。由于它们中没有人能够令人满意地预测整个静态速度范围内的空隙率,因此成功实施了漂移通量模型。最终,通过测量的压力梯度和空隙部分,实现了双流体模型以确定界面剪切应力并与文献的结果进行比较,强调操作条件对预测性能的影响。

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