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入渗

n.infiltration; influent seepage
网络infiltrate; soil water infiltration; unsaturated infiltration groundwater

入渗

英-汉网络释义

入渗

infiltration

1.入渗(Infiltration):地面上的雨水经由土壤渗入地面下. (1) 入渗率:单位时间由地表渗入土壤之雨水量,单位:mm/hr或mm/min (2) …

infiltrate

地下水可以入渗（infiltrate）或漏入到该系统中。当下水道系统入孔位置较低时，可能会有雨水通过入孔盖人流（inflow）进入 …

soil water infiltration

matrix potential of soil water_翻译 ... 土壤水： Soil water 入渗： soil water infiltration 水土： water and soil ...

unsaturated infiltration groundwater

成功大学电子学位论文服务 ... 李明浩 Ming-Hao Lee 入渗未饱和层地下水 unsaturated infiltration groundwater ...

surf ace spreading

回灌方式包括地表入渗 ( surf ace spreading) 、土壤含水层处理系统 ( SAT ) 、包气带注入回灌( vadose zon e injection) 以...

run-on

模型中，为考虑上游坡地单元入流的径流入渗(run-on)效应，在进行坡地产流计算时，降雨及上游坡面流及壤中出流被同时作为 …

QAll

水管之稳定入渗 (QAll)可表示为: QAll =QBOTTOM+2QSIDE (3-11) ;QBOTTOM=KsoilABOTTOM perc (3-12) ;QSIDE=0.5Ksoil…

例句：

The paleosol with less porosity did not develop well in water bearing space and was prone to form a water-resisting layer .

结果表明，黄土层含水空间发育好，入渗率较大，利于构成含水层；

Rainwater may infiltrate more easily with a higher initial soil water content and a deeper surface pond.

初始含水量越高和地表积水越深越利于雨水的入渗。

There was good linear relationship between the amount of cumulative infiltration and the wetting front distance .

累积入渗量与湿润锋推进距离呈良好的线性关系；

The role of grass land for increasing infiltration and reducing soil , water and solute loss is better than the trees.

荒草地减缓坡地径流、增加降雨入渗、减少土壤和养分流失效果明显优于灌木类（钙果）；

Both initial infiltration rate and final infiltration rate of south slope were higher than those of north slope on bare-slope .

而荒坡地的初始入渗速率和最终入渗速率均是阴坡高于阳坡。

The results showed that the rainfall infiltration features have significant difference among different land use types on purple soil .

结果表明，紫色土不同土地利用方式下降雨入渗过程差异显著。

stemflow altered the spatial pattern of rainfall below the canopy, influenced infiltrating water and conservation of water supply .

而树干流改变降雨水平空间格局，影响水分入渗以及土壤水源涵养。

Through the experiments on non-pressure irrigation , the text studied the influence of irrigation water volume to water movement .

通过试验，分析研究了不同灌溉水量对无压灌溉入渗过程中水分运移的影响。

The results showed that infiltration ability of non-water-repellent soils increased with the increase of mineralization degrees.

结果表明，不斥水土壤的入渗能力随矿化度的增加而增加。

The soil water infiltration in alkali-spot land is very low , so moved-down salts are much less than those moved up .

碱斑地土壤水分入渗率低，下行盐分远远小于上行盐分。

Under the same soil texture , as antecedent soil moisture increased, infiltration rate decreased and runoff intensity increased.

结果表明：土壤质地对入渗和径流过程有较大影响。

At length , the effect of the said fields change on the stability of slope is analyzed combining with engineering living example.

最后，结合工程实例分析了降雨入渗后渗流场的变化对土坡稳定性的影响。

入渗

入渗