saline infiltration 中文意思是什麼
saline infiltration
解釋
鹽類浸潤- saline : adj. 1. 鹽的；含鹽的；鹽性的，鹹的。2. 鹽漬的；【醫學】鹽水注射人工流產法。n. 1. 鹽沼，鹹湖，鹽泉；鹽皮；鹽咸灘；鹽田，鹽地，制鹽所，鹽場。2. 【醫學】鹽水；含鹽瀉藥。
- infiltration : n. 1. 滲入；【醫學】浸潤。2. 【軍事】滲透，通過；滲透活動。3. 【化學】滲濾。
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The results made clear that soil salt increased after saline water infiltration and decreased after fresh water infiltration
結果表明，不同輪灌條件下，土壤含鹽量隨灌溉鹹水而增加，隨淡水灌溉而降低。 -
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。 -
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律的室內模擬試驗研究，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於土壤初始含鹽量，中間土層基本保持土壤初始含鹽量值，但濕潤鋒附近發生突變，含鹽量達最大值。
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