| 点源入渗土壤水分运动规律实验研究 |
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| 引用本文： | 汪志荣,王文焰,王全九,张建丰.点源入渗土壤水分运动规律实验研究[J].水利学报,2000,31(6):0039-0045. |
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| 作者姓名： | 汪志荣 王文焰 王全九 张建丰 |
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| 作者单位： | 西安理工大学水资源研究所;西安理工大学水资源研究所;西安理工大学水资源研究所;西安理工大学水资源研究所 |
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| 摘 要： | 由不同质地土壤的点源入渗实验，得出了在不同滴头流量情况下，实际滴灌可以形成两种入渗边界，边界一是非充分供水点源入渗边界；边界二为变边界积水点源入渗边界。本文对两种边界条件特点及其滴头流量、灌水时间、湿润锋、含水量分布等之间的关系进行了分析，认为湿润比可以作为确定滴灌灌水参数的指标之一，对于实验滴灌的适宜湿润比以小于1.0为宜。
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| 关 键 词： | 点源 变边界积水 湿润比 入渗 |
| 文章编号： | 0559-9350(2000)06-0039-06 |
| 修稿时间： | 1999年5月12日 |
Experimental study on soil water movement from a point source |
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| WANG Zhirong,WANG Wenyan,WANG Quanjiu,ZHANG Jianfeng.Experimental study on soil water movement from a point source[J].Journal of Hydraulic Engineering,2000,31(6):0039-0045. |
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| Authors: | WANG Zhirong WANG Wenyan WANG Quanjiu ZHANG Jianfeng |
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| Affiliation: | 1.Xi'an University of Technology |
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| Abstract: | The infiltration experiment of point source irrigation reveals that two kinds of boundary condition may occur, depending on the drip flux. One is non-pond infiltration formed by insufficient flux, whereas another is pond infiltration with moving boundary. The characteristics of these two boundary conditions and the relationships among drip flux, irrigation duration, wetting front and distribution of soil moisture are analyzed in this paper. It concludes that the wetting front rate is one of the important parameters of drip irrigation and the best rate in less than 1.0. |
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| Keywords: | drip irrigation point source infiltration wetting front rate moving boundary |
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