infiltrated water 中文意思是什麼
infiltrated water
解釋
滲入的水- infiltrated : 浸潤的
- water : n 1 水；雨水；露；〈常作 pl 〉 礦泉，溫泉；藥水。2 〈常 pl 〉水體；水域；水道；海；湖；河；海域；...
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The percentage of preferential flow flux over the total infiltrated water can reach 2. 40 % ~ 48. 72 %
優先流水分通量最大可達剖面滲流水分通量的17200倍，會在很大程度上增加土壤水分運動通量。 -
In addition, bare land covered with weed would delay runoff - yielding time, increase infiltrated water, and make soil water move deeper
裸地坡面覆蓋雜草，能延緩產流時間、增加入滲，並促進土壤水分向深層的運移。 -
( 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 ）在以土壤水分消耗為主的時期，土壤蒸發時水分的整體移動性能較強，最大蒸發蒸騰作用層深度很快形成，並不是一個「由淺而深」的漸進過程。 -
( 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 ）在防止蒸發條件下，再分佈過程中，土壤水分在重力的作用下有沿坡向下運移的趨勢；在蒸發條件下，由於初始含水量一般較低，雨季量小且分散的降雨極易為強烈的蒸發蒸騰所消耗，側向沿坡向下流難以發生，但在持續的降雨條件下，土壤水分在重力勢和基質勢梯度的作用下易沿坡向下運移。 -
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較高的原因，可能主要與其蒸散較小且坡度較緩導致入滲水量較多有關；但是對于植被覆蓋度較低的坡地（如裸地） ，坡中下部土壤水分含量較高還與上方來水有較大的關系。 -
The results indicated that even if there was different at initial soil condition, such as initial moisture content and initial salt content, salt content in soil profile and sar at top soil increased greatly after the high salinity water infiltrated
結果表明盡管土壤初始條件存在差異，但灌高礦化度水后，土壤含鹽量和溶液濃度總體增加，且土壤剖面特別是表層的sar明顯增大。 -
The maximal preferential flow flux can reach 17200 times of that of infiltrated flow, which could increase soil water flux to a great extent
在同場降雨中，優先流的介入使得滲流流量峰值出現時間提前。 -
When the saline water ( < 3g / l ) infiltrated to 45cm, the top soil of 0 - 37cm was desalinized, when the saline water of 3g / l infiltrated, the desalinized depth was 0 - 15cm. moreover, sar of top soil increased with the sar of the infiltration water. 3. through lab experiment, the characteristics of soil water and salt movement under different initial soil moisture content were analyzed
當濕潤深度為45cm時，小於3g l的微鹹水入滲后， 0 - 37cm土層處于脫鹽狀態，而3g l的微鹹水入滲， 0 - 15cm土層處于脫鹽狀態， 15cm - 35cm土層含鹽量基本等於初始含鹽量，但濕潤鋒處含鹽量很高。
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