infiltration water meaning in Chinese
渗入水
渗透水
下渗水
Examples
- The results indicated that the higher the salinity of infiltration water was , the faster cumulative infiltration and wetting front increased , and more salt accumulated at the wetting front
入渗水的矿化度越高，土壤剖面含盐量越高，且湿润锋附近积聚的盐分越多。 - 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
当湿润深度为45cm时，小于3g l的微咸水入渗后， 0 - 37cm土层处于脱盐状态，而3g l的微咸水入渗， 0 - 15cm土层处于脱盐状态， 15cm - 35cm土层含盐量基本等于初始含盐量，但湿润锋处含盐量很高。 - The results were as follows : 1 . on the basis of saline water infiltration , the characteristics of movement of soil water and salt under different cumulative infiltration were studied . the results indicated that when the salinity of the infiltration water was 3g / l , the top soil was desalinized and salt accumulated at the wetting front
通过对不同入渗水量下土壤水盐运移规律的室内模拟试验研究，结果表明利用矿化度为3g l水入渗后，土壤从上至下逐渐脱盐，上层土壤含盐量略低于土壤初始含盐量，中间土层基本保持土壤初始含盐量值，但湿润锋附近发生突变，含盐量达最大值。 - Abstract : based on the data obtained from field observations and deformation monitoring , this paper deals with the deformation and failure of a double - decked slope composed of soft rock strata in its lower part and hard - brittle rock strata in its upper part . it is demonstrated that the deformation of this kind of slopes is always initiated by the non - homogeneous rheological compression of the lower soft rock strata , leading to the tension fracture and toppling of the upper hard rock strata , and at last the sliding of the whole deformed body will be caused by the shear failure along the stress - concentration zone in the lower soft rock mass under the actions of the gravitational loading and infiltration water
文摘:以现场考察和变形监测资料为依据，探讨一个下部有软弱基座，上部为硬脆性坡体的“二元结构”边坡的变形破坏问题，揭示这类边坡的变形总是以下部软弱岩体的不均匀压缩流变为先导，进而引起上部硬脆性坡体的拉裂与倾倒，最终通过渗入水的作用，使下部承载状况已进一步恶化了的软弱岩体，沿剪应力集中带发生剪切破坏而导致整个变形坡体的下滑。 - It is found that the degree of mineralization and metamorphic coefficient and conversion potential of formation water , the fault is zone of sluicing of atmospheric infiltration water flowing from basin west margin to east ( centripetal flow ) and sedimentary compaction water flowing from qija gulong depression to west ( centrifugal flow )
通过地层水矿化度和变质系数等参数的分布规律及一系列折算水位剖面图的分析发现，该断裂对水是不封闭的，并且是盆地西缘大气渗入水向东流动（向心流）及齐家古龙坳陷沉积压实水向西流动（离心流）的共同泄水带。