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Physically based closed-form expression for the bimodal unsaturated hydraulic conductivity function

机译:双峰不饱和导水率函数的基于物理的闭合形式表达式

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摘要

Simulation of flow and contaminant transport through the vadose zone requires accurate parameterization of the soil hydraulic properties. This requirement is particularly important for soils with a complex structure. In the present study, a physically based closed-form expression for the bimodal unsaturated hydraulic conductivity function is proposed for soils with bimodal pore-size distribution. It combines the bimodal representation of the soil-water characteristic curve (SWCC) function of Liu with the conductivity representation model of Mualem. The proposed equations are defined by parameters that have physical significance, which can be related to the properties of the materials. Experimental data for the representation of bimodal SWCCs and corresponding hydraulic conductivity curves were used to demonstrate the applicability of the proposed functions. The proposed approaches resulted in good agreement with experimental data. These functions can potentially be used as an effective tool for identifying hydraulic porosities in mediums with a complex structure.
机译:模拟通过渗流带的流量和污染物传输需要对土壤水力特性进行精确的参数化。对于具有复杂结构的土壤,此要求尤其重要。在本研究中,针对具有双峰孔径分布的土壤,提出了基于物理的双峰不饱和导水系数函数的闭式表达式。它结合了Liu的土壤水特征曲线(SWCC)函数的双峰表示与Mualem的电导率表示模型。所提出的方程式由具有物理意义的参数定义,这些参数可能与材料的特性有关。用于表示双峰SWCC的实验数据和相应的水力传导率曲线用于证明所提出功能的适用性。所提出的方法与实验数据良好吻合。这些功能可以潜在地用作识​​别结构复杂的介质中液压孔隙率的有效工具。

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