The water retention curve is one of the essential links to study the soil water movement.
土壤水分特征曲线是土壤水分运动研究必不可少的环节之一。
A spatially-random network model by using measured pore morphology was then set up to simulate the pore scale flow processes, and to predict the soil water retention curve near saturation.
在此基础上建立了基于土壤孔隙形态学特征的随机网络模型，在孔隙尺度模拟了土壤中的水分运动过程，并预测了近饱和土壤水分特征曲线。
This indicates that the sandy soil water retention curve can be predicted by the fractal model for sandy soil water retention curve.
这一结果对于实际工作中根据风沙土壤颗粒大小分布的分形维数来预测沙漠风沙土壤水分特征曲线具有一定的指导意义。
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