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Modifications of the turbulent diffusion layer model for the condensation heat transfer under the presence of noncondensable gases

机译:不可冷凝气体存在下湍流扩散层模型对冷凝传热的修正

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The condensation heat transfer model of the MARS-KS1.5 code tends to under-predict the condensation in the presence of noncondensable gases. In our previous study, we adopted the diffusion layer model and modified it in order to consider the effect on turbulence on diffusive mass transfer in the diffusion layer. In this work, further modifications were made by introducing the boundary layer theory for natural convection flow.The new condensation model has been validated against 442 experimental data collected from eight different facilities. It is shown that the results of the new model for natural convection flow are more accurate result than those of the previous model. It is confirmed that the new model works well for the condensation in forced convection flow. The relative root mean square error of the new model is reduced to 0.193 from 0.242 of the previous model and 0.401 of the original one. (C) 2019 Elsevier Ltd. All rights reserved.
机译:MARS-KS1.5代码的冷凝传热模型往往会在存在不可冷凝气体的情况下低估冷凝。在先前的研究中,我们采用了扩散层模型并对其进行了修改,以考虑湍流对扩散层中扩散质量传递的影响。在这项工作中,通过引入自然对流流动的边界层理论进行了进一步的修改。新的冷凝模型已经针对来自八个不同设施的442个实验数据进行了验证。结果表明,新模型的自然对流流动结果比以前的模型更为准确。可以肯定的是,该新模型对于强制对流中的凝结效果很好。新模型的相对均方根误差从先前模型的0.242和原始模型的0.401降低到0.193。 (C)2019 Elsevier Ltd.保留所有权利。

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