1) steady infiltration rate
稳渗率
1.
The surface stratum and the bottom of ploughed stratum of Yucheng experimental station being taken as investigated area,the steady infiltration rate fc and infiltration experiential index α are measured at about ninety-seven points.
以禹城综合试验站典型农田地块为研究对象,测得102 m×52 m面积内地表层与犁底层两个层面不同水平位置的土壤稳渗率f c与入渗经验指数α。
2.
An infiltration calculation solution for the soil with sand inter layer, including the time when nonlinear infiltration transmits into the steady infiltration and the steady infiltration rate, was developed based on the Lab experimental data and exiting infiltration equations.
根据室内系统的试验研究,对土壤具有砂质夹层的入渗计算问题,即非线性入渗阶段转为稳渗阶段时间与稳渗率,提出了一个以现有均质土积水入渗公式为基础的计算方法。
2) stable infiltration rate
稳渗率
1.
The results show that the main factors for finger flow occurrence are the stable infiltration rate and the saturated hydraulic conductivity of the sand layer.
研究表明:决定砂质双层结构能否发生指流现象的重要因素,一是入渗水流进入砂层后的稳渗率;二是表征砂层物理特性的饱和导水率;并以二者的比值做为判断发生指流现象的一个重要量化指标。
3) 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。
4) stable infiltration rate
稳定入渗率
1.
therefore,muddy water cumulative infiltration and stable infiltration rate decreases with increasing of sediment content in the .
对试验结果进行分析后表明:在相同入渗条件下,浑水入渗主要受泥沙含量的影响,由于入渗浑水中的泥沙入渗时在地表形成一个沉积层,因而对入渗起到阻碍作用,使得浑水累积入渗量和稳定入渗率都随浑水泥沙含量增大而减小;浑水入渗也符合Kostiakov-Lewis入渗模型,入渗指数随浑水泥沙含量的增大而增大,入渗系数和相对稳定入渗率随浑水泥沙含量的增大而减小。
2.
The stable infiltration rate is about 0.
结果表明:荒漠灌木-梭梭根区的稳定入渗率与孔隙度具有随着距离树干的增加而迅速下降,这一关系可用指数函数表示,沙垄间:K=3。
5) Stable water infiltration
土壤稳渗率
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