infiltrating water meaning in Chinese
入渗水
Examples
- The percentage of preferential flow flux over the total infiltrated water can reach 2 . 40 % ~ 48 . 72 %
优先流水分通量最大可达剖面渗流水分通量的17200倍，会在很大程度上增加土壤水分运动通量。 - In addition , bare land covered with weed would delay runoff - yielding time , increase infiltrated water , and make soil water move deeper
裸地坡面覆盖杂草，能延缓产流时间、增加入渗，并促进土壤水分向深层的运移。 - ( 7 ) during the process of water consumption , soil water almost lost from the whole profile . the great depth that resulted from evapotranspiration formed soon , but not gradually . infiltrated water was mostly consumed by evapotranspiration during ra
( 7 )在以土壤水分消耗为主的时期，土壤蒸发时水分的整体移动性能较强，最大蒸发蒸腾作用层深度很快形成，并不是一个“由浅而深”的渐进过程。 - ( 3 ) when evaporation was stopped during the process of soil water redistribution , soil water would move downslope by gravity . when evaporation was in process , due to low initial water content , most infiltrated water from small intensity and amount of rainfall would be consumed by intensive evapotranspiration during rainy season , and lateral downslope unsaturated flow seldom took place . however , soil water would move downslope by gravitational and matric potential gradients after continuous rainfall
( 3 )在防止蒸发条件下，再分布过程中，土壤水分在重力的作用下有沿坡向下运移的趋势；在蒸发条件下，由于初始含水量一般较低，雨季量小且分散的降雨极易为强烈的蒸发蒸腾所消耗，侧向沿坡向下流难以发生，但在持续的降雨条件下，土壤水分在重力势和基质势梯度的作用下易沿坡向下运移。 - The middle and lower parts of woodland and grassland had higher soil water contents during rainy season , which resulted from smaller evapotranspiration and more infiltrated water with a lower gradient . however , upslope runoff infiltration was another reason for hillslope with a lower cover ratio , such as bare land
雨季林草地坡中下部土壤水分含量较高的原因，可能主要与其蒸散较小且坡度较缓导致入渗水量较多有关；但是对于植被覆盖度较低的坡地(如裸地) ，坡中下部土壤水分含量较高还与上方来水有较大的关系。