首先，评述了现有的测定和确定单裂隙非饱和水力参数的几种方法的优缺点，为单裂隙非饱和水力参数的确定提供了理论依据。
Firstly, the advantages and disadvantages of present measurement and determination methods of unsaturated hydraulic parameters for a single fracture are commented upon.
土壤水力性质是研究非饱和带中水分和溶质运移的重要参数，可以用孔隙网络模型进行预测。
Soil hydraulic properties are the key information required in quantitatively modeling water flow and solute transport in the vadose zone, which can be predicted using pore scale network models.
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