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| 负水头供水条件下土壤水分一维入渗规律的研究 | |
| 引用本文： | 解迎革,薛绪掌,王国栋,李霞.负水头供水条件下土壤水分一维入渗规律的研究[J].干旱地区农业研究,2007,25(5):119-124. |
| 作者姓名： | 解迎革 薛绪掌 王国栋 李霞 |
| 作者单位： | 1. 国家农业信息化工程技术研究中心,北京,100089;西北农林科技大学理学院,陕西,杨凌,712100 2. 国家农业信息化工程技术研究中心,北京,100089 3. 西北农林科技大学理学院,陕西,杨凌,712100 |
| 基金项目： | 国家自然科学基金 , 北京市科技新星计划项目 |
| 摘 要： | 将土壤供水头压力控制为负值,测定了垂直入渗、毛管上升和水平入渗3种情况下的土壤吸水过程.发现随供水吸力的增加,垂直入渗、毛管上升和水平入渗过程中湿润峰前进速度和入渗速度的相对差异变小.将入渗速率等于潜在蒸发速率时的湿润厚度定义为临界湿润厚度,计算了潜在蒸散宰为5 mm/d时不同负水头下壤土的临界湿润厚度;确认了垂直、毛管和水平入渗下湿润峰位置与入渗量的关系,将湿润蜂位置-累计入渗量曲线的斜率,印巴湿润土体内入渗水分所占的容积百分数定义为湿润系数,提供了所测壤土的湿润系数-负水头曲线;建立了负水头供水过程中土壤含水量空间分布模型;观察到湿润锋含水量与供水吸力闸的依赖关系. |
| 关 键 词： | 土壤水分 负水头 入渗 毛管上升 湿润锋 |
| 文章编号： | 1000-7601（2007）05-0119-06 |
| 修稿时间： | 2006-12-16 |
One-dimensional soil water infiltration under water supply of negative hydraulic heads |
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| XIE Ying-ge,XUE Xu-zhang,WANG Guo-dong,LI Xia.One-dimensional soil water infiltration under water supply of negative hydraulic heads[J].Agricultural Research in the Arid Areas,2007,25(5):119-124. | |
| Authors: | XIE Ying-ge XUE Xu-zhang WANG Guo-dong LI Xia |
| Abstract: | Hydraulic head of supply water is maintained at negative values and vertical infiltration,capillary rise,and horizontal infiltration processes were observed.With increasing water supply tensions,relative differences of vertical infiltration,capillary rise,and horizontal infiltration processes in infiltration rates and wetting front movement speed decreased.The wetting depth at which infiltration rate is equal to potential evapo-transpiration rate is defined as critical wetting depth,and critical wetting depths at different negative hydraulic heads were obtained for the studied loamy soil by setting potential evapotransporation rate at 5 mm/d.Linear relationships between wetting depth and cumulative infiltration amount for vertical infiltration,capillary rise,and horizontal infiltration were validated.The slope of wetting depth-cumulative infiltration,i.e.,percentage of wetted soil volume occupied by infiltrated moisture,was defined as wetting coefficient,and the relationships between wetting coefficient and supply hydraulic head were provided for the studied loamy soil.A model describing soil moisture profile for vertical infiltration,capillary rise,and horizontal infiltration under negative supply hydraulic head was provided.The reliance of wetting front water content on supply hydraulic head was also demonstrated. |
| Keywords: | soil water negative hydraulic head infiltration capillary rise wetting front |
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