infiltration water造句
例句與造句
- 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
入滲水的礦化度越高,土壤剖面含鹽量越高,且濕潤鋒附近積聚的鹽分越多。 - 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
當濕潤深度為45cm時,小于3g l的微咸水入滲后, 0 - 37cm土層處于脫鹽狀態(tài),而3g l的微咸水入滲, 0 - 15cm土層處于脫鹽狀態(tài), 15cm - 35cm土層含鹽量基本等于初始含鹽量,但濕潤鋒處含鹽量很高。 - 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
通過對不同入滲水量下土壤水鹽運移規(guī)律的室內(nèi)模擬試驗研究,結果表明利用礦化度為3g l水入滲后,土壤從上至下逐漸脫鹽,上層土壤含鹽量略低于土壤初始含鹽量,中間土層基本保持土壤初始含鹽量值,但濕潤鋒附近發(fā)生突變,含鹽量達最大值。 - 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:以現(xiàn)場考察和變形監(jiān)測資料為依據(jù),探討一個下部有軟弱基座,上部為硬脆性坡體的“二元結構”邊坡的變形破壞問題,揭示這類邊坡的變形總是以下部軟弱巖體的不均勻壓縮流變?yōu)橄葘ВM而引起上部硬脆性坡體的拉裂與傾倒,最終通過滲入水的作用,使下部承載狀況已進一步惡化了的軟弱巖體,沿剪應力集中帶發(fā)生剪切破壞而導致整個變形坡體的下滑。 - 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 )
通過地層水礦化度和變質(zhì)系數(shù)等參數(shù)的分布規(guī)律及一系列折算水位剖面圖的分析發(fā)現(xiàn),該斷裂對水是不封閉的,并且是盆地西緣大氣滲入水向東流動(向心流)及齊家古龍坳陷沉積壓實水向西流動(離心流)的共同泄水帶。 - It's difficult to find infiltration water in a sentence. 用infiltration water造句挺難的