1) soil water leakage
土壤水分渗漏
1.
On the basis of field investigation and former studies,analysis after using organism timing water,the change of soil water content rate,soil moisture evaporation,soil water leakage and water absorption to plants.
根据实地测定和前人研究成果,分析了施放生物定时水后土壤含水率、土壤水分蒸发、土壤水分渗漏及植物水分吸收关系,推导出造林植物需补充水量的公式,为生物定时水的造林应用提供理论依据。
2) soil water percolation
土壤水渗漏
1.
Soil nitrogen loss is highly relevant to the soil water leakage and percolation,and soil water percolation is further driven by the rainfall condition at the soil surface.
为了揭示土壤水渗漏对不同降雨条件的响应规律,采用数值模拟方法模拟了不同降雨情景下土壤水渗漏量的变化,并与实际降雨条件下现场观测结果进行比较。
3) Nutrient change of soil percolating water
土壤渗漏水养分变化
4) soil water percolation rate
土壤水渗漏率
5) soil percolation
土壤渗漏
1.
Soil moisture includes percentage of soil moisture,soil evaporation and soil percolation.
土壤水分包括土壤含水率、土壤蒸发、土壤渗漏3个方面的内容,互相影响,互相制约。
6) soil water infiltration
土壤水分入渗
1.
Based on soil water infiltration experiments in corn field, this paper analysed and discussed yearly change characteristics of soil water infiltration .
以大田玉米地的土壤水分入渗跟踪试验为依据 ,分析讨论了土壤水分入渗的年变化特性 ,结果表明 ,给定土壤质地 ,土壤结构由疏松变密实 ,土壤水分入渗能力逐渐减小 ,土壤含水率的变化引起土壤水分入渗能力上下变幅。
2.
The soil saturated hydraulic conductivity Ks of BSC and three types of control(no any crust,physical crust and removed BSC) were measured by tension infiltrometer to explore the effects of BSC on soil water infiltration and conductivity.
另一方面,与不同的对照相比,生物结皮对土壤饱和导水率的影响截然不同,该结论可在一定程度上解释当前有关生物结皮影响土壤水分入渗方面所存在的分歧。
补充资料：土壤水分运动基本方程(见土壤水运动)
土壤水分运动基本方程(见土壤水运动)
turang shuifen yundong iiben土壤水分运动基本方程fangeheng见土壤水运动。
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