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Numerical simulation of the transport of water in soil with macropores

机译:大孔隙水在土壤中运移的数值模拟

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Exact description of water movement in soil needs a model that can reflect the physical character of the soil. In this paper, we assume that soil is divided into two porous media, one for matrix flow and one for macropore flow. A macropore is assumed to extend vertically from the soil surface down to the desired depth.Macropore density is also incorporated into the model to describe the complex distribution of macropores in soil. Water movement in the two flow domains is simulated using different models. In order to improve the computational efficiency, the domain decomposition method is adopted. From the comparison of the simulation results, it can be seen that the models and methods that are used in this research can depict the characteristic of macropore flow and improve the practicability and applicability of the model.
机译:对土壤中水运动的精确描述需要一个能够反映土壤物理特性的模型。在本文中,我们假设土壤被分为两种多孔介质,一种用于基质流,另一种用于大孔流。假定大孔从土壤表面垂直向下延伸至所需深度。模型中还包含了大孔密度,以描述大孔在土壤中的复杂分布。使用不同的模型模拟了两个流域中的水运动。为了提高计算效率,采用了域分解法。从仿真结果的比较可以看出,本研究中使用的模型和方法可以描述大孔流动的特征,提高模型的实用性和适用性。

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