高鹽水含水層 的英文怎麼說

中文拼音 [gāoyánshuǐhánshuǐcéng]
高鹽水含水層 英文
highly saline aquifer
  • 高 : Ⅰ形容詞1 （從下向上距離大; 離地面遠） tall; high 2 （在一般標準或平均程度之上; 等級在上的） above...
  • 鹽 : 名詞1. （食鹽; 鹽類） salt 2. （姓氏） a surname
  • 水 : 名詞1 （由兩個氫原子和一個氧原子結合而成的液體） water 2 （河流） river 3 （指江、河、湖、海、洋...
  • 含 : 動詞1 （東西放在嘴裏 不咽下也不吐出） keep in the mouth 2 （藏在裏面; 包含） contain 3 （帶有某種...
  • 層 : i 量詞1 （用於重疊、積累的東西 如樓層、階層、地層） storey; tier; stratum 2 （用於可以分項分步的...
  • 鹽水 : saline water; salting liquor; salt solution; brine solution; brine鹽水精製 salt refining; 鹽水選...
  1. In many sedimentary basins the salinity of the formation water increases with depth or compaction.

    在許多沉積盆地中，地層水的含鹽量隨深度或壓實作用而增高。
  2. The high content and the high water temperature favour the solution of salt and metals from the underground formations.

    高含量和高水溫促進了地下巖層里鹽類和金屬的溶解。
  3. 4 ) the characteristic of tricyclic terpane reflected the source input of algae. the predominance of 4 - methylsterane and dinosterane, and the c _ ( 27 ) - sterane predominance " v " distribution pattern all indicate the great contribution of algae source input. based on the ratio of sterane c2920s / ( 20s + 20r ) and c29 / ( + ), the source rocks can be regarded as typical immature source rocks

    2 、利用豐富的生物標志化合物信息，分析解釋了生源構成、沉積環境、有機質演化等特徵，表明德南窪陷主力烴源巖的生源構成是以菌藻類微生物為主且含有一定陸生植物輸入的混合生源，沉積環境為半鹹水-鹹水還原環境，沉積水體具有「層狀」特點，表層鹽度高，底層還原性強。
  4. Tianjin is located at north part of northern china plain, where is rich in thermal water in sedimentary basin. the main reservoir is carbonate rocks of the paleozoic and upper and middle proterozoic group, which contain thermal waters with temperature of more than 90. the cap rock is cenozoic sedimentary rocks with thickness of more than 1000m, which contains thermal water with temperature from 25 to 70 in 13 sandstone layers. the temperature of thermal water is steady growth along with the deepen of basin. all thermal waters in different aquifers are medical mineral waters, which is conducive to good health

    天津位於華北平原的北部，那裡的沉積盆地含有豐富的地下熱水。主要的熱儲層為古生界和上中元古界的碳酸鹽巖層，所含熱水的溫度略高於90蓋巖層為新生界沉積層，在13個砂巖含水層中含有2570的熱水。熱水的溫度隨盆地深度的增加而增加。
  5. 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。
  6. 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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