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Model of water-air two-phase flow in saturated-unsaturated soil

机译:饱和不饱和土壤中的水 - 空气两相流模型

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For seepage in unsaturated soil, there are both air flow and water flow, which can be called the water-air two-phase flow. In order to simulate the water-air two-phase flow in soil when there is groundwater, a numerical model of water-air two-phase flow in saturated-unsaturated soil is established in this paper. By the model, the air-flow and water-flow in unsaturated soil are both considered in seepage calculation. And the mass transfer between air-phase and water-phase, change of phase states are considered in calculation. Capillary pressure is the most important factor for the water-air two-phase flow in unsaturated soil, and the calculation method of capillary pressure is also given in the paper. At last examples are given to verify the correctness of the numerical model and the calculation method.
机译:对于在不饱和土壤中的渗漏,空气流量和水流都可以称为水 - 空气两相流。为了在地下水中模拟土壤中的水中两相流,在本文中建立了饱和不饱和土壤中的水 - 空气两相流量的数值模型。通过模型,在渗流计算中考虑不饱和土壤中的气流和水流。在计算中考虑了空移与水相之间的传质变化,在计算中考虑了相态的变化。毛细管压力是不饱和土中的水 - 空气两相流动的最重要因素,纸张中还给出了毛细管压力的计算方法。在最后的示例中,给出了验证数值模型的正确性和计算方法。

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