1) infiltration intensity
下渗强度
1.
Accordingto the condition at the interface, the formula for calculating the infiltration intensity is obtained and much more simpler in shape and easier in calculation than that used in previous studies.
论证了稻田土层剖面上出现非饱和流动区域的三个主要水力特征,并证明了在负压水头逐渐坛大区(A区)与负压水头逐渐减小区(B区)间存在一个压力水头梯度为零、下渗水流仅在重力作用下的层面,并以此为条件推导出下渗强度q的简化计算式。
2) depth of infiltration
下渗深度
1.
The relations between rainfalls, contents of soil water before rainfall, time of infiltration and depth of infiltration were described.
分析了不同雨量条件下刺槐林地土壤水分下渗过程，得出不同雨量下的土壤水分下渗深度即稳定渗深。
3) steady seepage intensity
稳渗强度
4) infiltration intensity
入渗强度
5) anti-permeability strength
抗渗强度
1.
Probability model distribution of permeability coefficient and anti-permeability strength of sand;
粗砂渗透系数与抗渗强度概型分布
6) seepage rate
渗漏强度
1.
Study on NH￣+_4-N transformation and movement in flooding paddy soil under different seepage rate;
不同渗漏强度条件下淹水稻田中氨态氮转化和运移的研究
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。
参考词条