含水土层 [
hán shuǐ tǔ céng]
aquifer
aquiclude
- 地下水循环系统由含水土层补水和排水和含水土层系统的结构控制。
The growth of the groundwater flow system is controlled by recharge and discharge of the (aquifer) and structure of the (aquifer) system. - 在100深的地下含水土层,热水会进入一系列业已敷设好的热交换器去加热地下水。
About 100 metres down lies a natural aquifer into which a series of heat exchangers have been built. - 在很多地方,随著乾旱的恶化、雨周期的改变、及高山溶雪的减少,河川、泊、及含水土层的蓄水量可能会因此减少。
shifting rainfall patterns and dwindling runoff from snow and ice in mountains may badly deplete rivers, lakes and aquifers.
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