非饱和土壤水一维流动的数值计算
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NUMERICAL METHOD OF ONE-DIMENSIONAL FLOW THROUGH UNSATURATED SOILS
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    摘要:

    非饱和土壤水的流动是指土壤中水分未充满全部孔隙时的水分移动而言的,是多孔介质中流体运动的一种重要形式。由于它在土壤科学、水文学、农田灌溉和排水、水资源评价等方面甚为重要,所以愈为人们所重视。

    Abstract:

    The present paper deals with a matrix equation for one,dimensional flow through unsaturated soil derived from the finite element method and a BASIC Program which has been applied to solve the problem of lateral seepage in soil in a DJ-130 computer.Better agreement is observed between the results obtained from the equation and the data from exPeriment as well as Philip's analytieal and quasi-analytieal solution,and the program is Proved applieable.With the aid of this progrem,the rate of lateral seepage,the relationship between wetting front and time,the vertieal infiltration upward from ground-water table and that downward from wetted soil surfaoe are computed and discussed preliminarily.

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雷志栋,杨诗秀.非饱和土壤水一维流动的数值计算[J].土壤学报,1982,19(2):141-153. Lei Zhi-dong, Yang Shi-xiu. NUMERICAL METHOD OF ONE-DIMENSIONAL FLOW THROUGH UNSATURATED SOILS[J]. Acta Pedologica Sinica,1982,19(2):141-153.

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  • 在线发布日期: 2013-02-25
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