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1)  final infiltration rate
稳渗速率
1.
By using a method of overflowing in a slope plot,a final infiltration rate on hillslopes under 4 typical vegetation forms and the influencing factors were investigated in the small watershed of Diediegou.
采用小区漫流法研究叠叠沟小流域内4种典型植被下的土壤稳渗速率及其影响因子。
2)  soil steady infiltration rate
土壤稳渗速率
1.
The results show runoff time has a negative relationship with soil bulk, antecedent soil moisture, slope gradient, rainfall intensity, and different tillage measures; soil steady infiltration rates have a positive relationship with rainfall intensity and tillage measures, and have a negative relationship with soil bulk, antecedent soil moisture, and slope gradient.
发现坡面产流历时与土壤容重、初始含水率、坡度、降雨强度、耕作管理措施呈负相关;土壤稳渗速率与降雨强度、耕作管理措施呈正相关,与土壤容重、初始含水率、坡度呈负相关。
3)  steady-state rate of permeation
稳态渗透速率
4)  steady water infiltration rates
稳定入渗速率
1.
This study mainly discuss the spatial interpolation uncertainty of soil steady water infiltration rates in Ji river basin which located in the third vice-area of loess hilly and gully region.
以黄土丘陵沟壑第三副区的藉河流域为研究区,根据65个实测点数据,采用普通克里格法、反距离权重法、样条函数法等插值方法,分析了测点数量变化、栅格像元尺寸变化及插值方法的差异对土壤稳定入渗速率空间插值结果的影响,剖析了空间插值中的不确定性。
5)  constant infiltration rate of soil
土壤稳定入渗速率
6)  infiltration capability
稳渗速度
补充资料:渗渗
1.寒冷貌。 2.指因害怕而产生发冷的感觉。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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