考虑膜流的低含水量传热非平衡相变分析

M. B. Kebre, F. Ouedraogo, B. Naon, F. Cherblanc, F. Zougmore
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引用次数: 1

摘要

考虑膜流的低含水量传热非平衡相变分析。摘要:本文通过考虑膜流对液态水运动的贡献,分析了低含水量条件下非平衡相变对沙质土壤水分转移的影响。事实上,大多数非平衡研究方法使用的是水力导电性,van Genuchten-Mualem (VGM)毛管模型,该模型没有考虑低含水量下的膜流动。因此,我们利用单向非平衡两相流模型进行了理论研究,模拟了液态水过滤和水蒸气扩散耦合液/气相变化的水传递。然后,我们将非平衡结果与考虑水力导率函数的经典VGM模型和考虑膜流的另一个模型进行了比较。数值模拟是基于暴露在受控大气中的沙土柱。我们观察到,用毛细管模型模拟的流体(液态水、液/气非平衡相变)的轮廓形状与考虑薄膜流动的模型所得到的形状有很大的不同。在最后一种情况下,液/气不平衡不像毛细管模型那样明显。似乎薄膜流动通过延迟相变过程来掩盖水蒸气的扩散,因此进入土壤的水蒸气浓度比单独考虑毛细流动的情况要低。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Analysis of Non-Equilibrium Phase Change in Transfers at Low Water Content by Considering the Film Flow
Analysis of Non-Equilibrium Phase Change in Transfers at Low Water Content by Considering the Film Flow. Abstract: In this study, we analyze the effect of non-equilibrium phase change on transfer at low water content in a sandy soil by considering the contribution of film flow in the motion of liquid water. Indeed, most of the non-equilibrium study methods use for hydraulic conductivity, the van Genuchten-Mualem (VGM) capillary model which does not consider the film flow occurred at low water contents. Thus, we conduct a theoretical study by using an unidirectional non-equilibrium two phase flow model to simulate water transfers by filtration of liquid water and diffusion of water vapour coupled by liquid/gas phase change. We then compare the results of the non-equilibrium with the classical model of VGM for hydraulic conductivity function and another model considering the film flows. The numerical simulation is based on a column of sandy soil exposed to a controlled atmosphere. We observe that the shapes of the profiles of fluxes (liquid water, liquid/vapour non-equilibrium phase change) simulated using the capillary model are very different from those obtained with the model considering the film flow. In this last case, the liquid/gas nonequilibrium is not noticeable as in the case of the capillary model. It seems that the film flows occult the water vapour diffusion by delaying the phase change process, therefore a lower concentration of water vapour into the soil than in the case where the capillary flow alone has been considered.
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