1)  unsaturated loess
包气带黄土
1.
It is shown from the results that moisture in shallow unsaturated loess moved obviously down and up as well as was poor in the semi-arid area.
研究结果表明 ,在半干旱地区的包气带黄土中 ,土壤浅部水的上下运动明显 ;降水的垂直入渗量甚小 ,最多约为降水量的 1 % ;而且降水的垂直入渗量随深度增加而减小。
2)  vadose zone
包气带
1.
Study on the migration and transformation of organic pollutants in vadose zone;
有机污染物在包气带中迁移转化试验研究
2.
Modeling study on transport law of leachate pollutant COD in vadose zones;
垃圾渗滤液有机污染组分在包气带中衰减规律的模拟研究
3.
An experimental study on residual saturation of diesel oil in vadose zone;
包气带柴油残余饱和度影响因素实验研究
3)  aeration zone
包气带
1.
Law of Vertical transfer of fly ash water in aeration zone of soil;
粉煤灰水在土壤包气带中的垂直迁移规律
2.
Biodegradability of heavy-oils in soil of an aeration zone;
包气带土层中重质油的生物可降解性
3.
A new technique of treatment and utilization of residential area rainwater was developed based on the characteristics of abundant soil water within aeration zone in southern cities, which can treat and utilize rainwater by means of primary precipitation and secondary biochemical treatment, to coo.
本研究根据南方地区包气带中土壤水丰富的特点,设计出一种新型小区雨水处理利用方法。
4)  unsaturated zone
包气带
1.
The adsorption of trichlorinated hydrocarbon in the unsaturated zone;
包气带对三氯乙烯的吸附行为研究
2.
Application of water solute coupled model to transportation of chemicals and pesticides on unsaturated zone pollution;
水质耦合模型在农药对土壤包气带污染中应用
3.
Lithologic characteristics of the unsaturated zone and its impact on adsorption and degradation of pesticide in the first grade terrace of Songhua River;
松花江一级阶地包气带岩性特征及其对农药吸附与降解的影响
5)  aerated zone
包气带
1.
Simulation experiments and forecast of migration and transformation of pollutants of leathate in aerated zone;
垃圾渗滤液中污染物在包气带运移模拟实验及预测
2.
Experimental study on effect of immobile water on solute transport in aerated zone of loess;
不流动水对黄土包气带溶质运移影响的实验研究
3.
Numerical modeling of ~(85)Sr migration in aerated zone with the characteristic of double peak concentration distribu-tion;
包气带中~(85)Sr迁移的浓度双峰分布数值模拟研究
6)  Aerated zone
包气层
参考词条
补充资料:包气带
包气带
aeration,zone of

   从地下水面到地面的地带。挖井时常见到井壁的上部往往是干的,含水很少。往下挖,井壁逐渐变湿,但井中仍然无水。再向下挖,井壁和井底有水渗出,井中很快形成水面,这便是地下水面。地下水面以上便是包气带,以下是饱水带。按水分分布特点,包气带可分成3个带:① 近地面段为毛细管悬着水带。这个带同大气有强烈的水分交换,水分的增加、减少或消失,同降雨的下渗、土壤的蒸发和植物的散发有关。水分的垂直分布随时间而变化。②毛细管支持水带。地下水面以上由毛细管水上升而形成,在这一带中土壤的含水量自下而上逐渐减少,这个带的深度随地下水位的升降而变化。③介于上述两个带之间的中间包气带。当地下水位深时,中间包气带一般水量较小,变化慢,垂直方向水分分布均匀。当地下水位浅时,毛细管悬着水带同毛细管支持水带连接起来,中间包气带随之消失。
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