2) oxygen in soil
土壤氧气
3) mercury vapor in soil
壤中气汞
1.
The pollution of Hg in air and mercury vapor in soil in Huangshi City was investigated and evaluated by Nemerow Comprehension method.
摘 要: 在对黄石市城市大气汞、土壤壤中气汞含量进行测定的基础上,采用内梅罗评价方法,对该地区的环境汞污染现状做了评价。
4) subsurface flow
壤中流
1.
Construction and application of a coupled slope surface-subsurface flow model for forested watershed;
森林流域坡面流与壤中流耦合模型的构建与应用
2.
The results showed that due to high annual precipitation and groundwater level near ground,subsurface flow of the farmland topsoil in Liuchahe watershed was very plentiful,but the flow volumes changed quickly with daily precipitati.
选取我国东部江淮丘陵地区典型小流域——六叉河流域为实验区,以流域主要土地利用类型——旱地土壤为研究对象,原位监测了作物整个生长期中,不同磷肥条件下,磷在旱地壤中流中水平空间差异、时间动态与土壤垂直差异上的动态迁移规律。
3.
The calculation of subsurface flow is the key to solve the problem because it is directly associated with simulation accuracy.
半干旱半湿润地区径流预报皆有超持与超渗的产流特征,是水文预报中的难点问题,而其中壤中流的计算又是关键,直接关系到模拟的精度。
5) Gas in soil
壤中气
6) subsurface runoff
壤中流
1.
The erosion characteristics,sediment yield mode,runoff generation process and the percentages of the surface runoff and the subsurface runoff accounting for the total pre.
结果表明:紫色土坡面总径流主要由地表径流和壤中流两种形式组成,地表径流和壤中流在总降雨量中的比例随雨强和坡度的不同而发生变化,在相同坡度情况下,壤中流占总降雨量的比例随雨强的减小而增大,在雨强相似的条件下,壤中流占总降雨量的比例随坡度的增大而增大。
2.
The objective of this study was to study the occurrence of subsurface runoff and the movement of.
壤中流以垂直入渗为主 ,并滞后于降雨 0 。
3.
The results show that the percentage of the subsurface runoff account for 0.
壤中流作为紫色土坡面一种产流形式,其引起的养分流失往往被忽视,针对这一问题,采用人工模拟降雨法,在3。
补充资料：壤壤
1.纷乱貌。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条