黄土中水分迁移规律现场试验研究

›› 2013, Vol. 34 ›› Issue (5): 1331-1339.

黄土中水分迁移规律现场试验研究

李萍¹，李同录¹，王阿丹²，张亚国²，梁燕³，赵纪飞¹

1. 长安大学地测学院地质工程系，西安 710054；2. 同济大学地下系，上海 200092； 3. 长安大学公路学院特殊地区公路工程教育部重点实验室，西安 710064

收稿日期:2012-07-05 出版日期:2013-05-10 发布日期:2013-05-14
作者简介:李萍，女，1988年生，硕士研究生，主要从事岩土工程方面的研究工作。
基金资助:
国家自然科学基金项目(No. 40972182，No. 41172256)

In-situ test research on regularities of water migration in loess

LI Ping¹，LI Tong-lu¹，WANG A-dan²，ZHANG Ya-guo²，LIANG Yan³，ZHAO Ji-fei¹

1. Department of Geological Engineering, School of Geological Engineering and Surveying, Chang’an University, Xi’an 710054, China; 2. Department of Geotechnical Engineering, Tongji University, Shanghai 200092, China; 3. Key Laboratory of Education Ministry on Highway Engineering of Special Region, School of Highway, Chang’an University, Xi’an 710064, China

Received:2012-07-05 Online:2013-05-10 Published:2013-05-14

摘要/Abstract

摘要： 黄土地区降雨诱发滑坡是不争的事实，但黄土地区地下水位很深，降雨入渗地面后如何运移，与地下水有无直接联系，目前还不是很清楚。为此设计了人工滴水试验模拟天然降雨条件，通过在一深度为10 m的探井井壁上埋设土壤水分计，观测人工滴水入渗过程中不同深度土体含水率随时间的变化情况，以确定其入渗影响深度。监测结果显示：降雨量为3.82 mm/d (小雨)时，0.5 m内土体含水率变化明显，0.5 m以下土层含水率几乎没有变化；降雨量为10.31 mm/d(中雨)时，1 m内土体含水率有所增加；降雨量达25.21 mm/d(大雨)时，1 m内土体含水率增长明显，1.0～1.6 m范围内有微弱增长；随着深度增加，土体含水率变化逐渐滞后，增幅逐渐减小。这说明在干旱的黄土地区，若无明显入水通道，短期内降雨的入渗深度有限，很难到达地下水位；但深部古土壤层的观测结果表明，即使在其上部黄土中含水率变化极其微弱的情况下，古土壤中的含水率上升明显，表明黄土中非饱和渗流或水汽迁移是存在的。通过试验还表明，陇东黄土高原地区土壤中水分循环主要发生在浅层0.7 m以内的蒸发带。降雨入渗到蒸发带以内，若无后续降雨补给，则向上蒸发排泄；若入渗至蒸发带以下，则不受蒸发影响，得以继续向下迁移；当遇到不透水面时，会在层面附近富集，有限元模拟也较好地反映了这一规律。

关键词: 土壤水分, 体积含水率, 入渗, 降雨, 黄土, 土-水特征曲线, 渗透系数

Abstract: It is an indisputable fact that rainfall can induce landslides in loess area; however, groundwater levels are always very deep in loess area. At present, it is not clear that how does rainfall move in loess and whether it affects groundwater directly when infiltrating ground below. In order to simulate the natural rainfall condition, manual drip experiment is carried out. By using soil moisture meters which are inserted into the wall at a 10 m-deep exploratory well, the changes of moisture content with time of soil layers at different depths in the process of artificial rainfall infiltration could be easily observed; the range affected by rainfall could be confirmed later. The result shows that moisture content of soil layers within 0.5 m changed obviously when the precipitation is 3.82 mm/d (light rain), while that of below have almost no changes; the moisture content within 1 m increases when the precipitation is 10.31 mm/d (moderate rain); the moisture content of the layers within 1 m increases significantly, and that of between 1 m to 1.6 m have a slight rise when the precipitation reached 25.21 mm/d (heavy rain), the changes of moisture content lag and the growth decreases gradually with depth. It is shown that if there are no obvious water paths in arid loess region, the infiltration depth of short-term rainfall is limited and it is difficult to reach the groundwater level, but according to the results of paleosol in deeper, the moisture content of paleosol has a considerable increase even though that of upper loess is relatively weak, which indicates that unsaturated seepage or vapor migration do exist in loess. It is also found that the circulation of soil moisture is primarily occurred in evaporation zone; that within shallow 0.7 m in Longdong Loess Plateau, if there is no recharge from follow-up rainfall, the rainfall infiltrated within evaporation zone will be excreted upward by evaporation; however, it will continue to move downward without the influence of evaporation when infiltrating beyond the evaporation zone; the water will gather on the surface as encountering the impervious layer, which is also reflected preferably by finite element simulation.

Key words: soil moisture, volumetric water content, infiltration, rainfall, loess, soil-water characteristic curve, permeability coefficient

中图分类号:

TU 411

李萍，李同录，王阿丹，张亚国，梁燕，赵纪飞 . 黄土中水分迁移规律现场试验研究[J]. , 2013, 34(5): 1331-1339.

LI Ping ，LI Tong-lu ，WANG A-dan ，ZHANG Ya-guo ，LIANG Yan ，ZHAO Ji-fei . In-situ test research on regularities of water migration in loess[J]. , 2013, 34(5): 1331-1339.

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