infiltration rate

基本解釋

The curve of soil infiltration rate with time is different greatly from that of normal infiltration in press.
隨著降雨雨型的變化，土壤入滲速率依時間變化曲線與常態(tài)有壓入滲時迥然不同。
The groundwater level above pipe bottom and anti-infiltration of pipe joint are the decisive factors affecting the groundwater infiltration rate.
管底以上的地下水位和管道接口的防滲施工質(zhì)量是地下水滲入量大小的決定性因素。
By indoor experiment this paper analysis the characteristic of the intermittent infiltration from infiltration amount, infiltration rate, wetting front and moisture content in soil.
通過室內(nèi)垂直一維積水入滲試驗(yàn)，從入滲量、入滲率、濕潤鋒、土壤含水量分布等方面分析了間歇入滲特性。

入滲速率
穩(wěn)滲率
Steady infiltration rate is an important parameter reflecting the soil permeability.
穩(wěn)定入滲率(穩(wěn)滲率)是衡量土壤滲透性能的重要指標(biāo)。
環(huán)境科學(xué)技術(shù)
入滲速率
The stability infiltration rate of the 10th paleosols(S10) is the lowest, which is about 0.08mm/min.
入滲速率最小的是第10層紅褐色古土壤(S10),為0.08mm/min。
滲水速率
滲透速率
滲濾速率