不节制的工业化, 尤其是在穷国, 正在污染河流和地下含水层们.
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There are three types of aquifers: perched, unconfined, and confined.
含水层有三种形态, 分别是上层滞水 、 潜水和承压水.
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So the risk of inadvertently contaminating the deep aquifers must be carefully weighed.
所以,深层含水层意外受污染的风险一定要小心考虑.
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探讨了四个突水含水层水文地球化学特征差异及原因.
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含水层的位置和范围是根据下垫岩石的地质条件所决定的.
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Water that infiltrates the soil and is located in underground reservoirs called aquifers.
浇灌渗入土壤且位于地下水库或蓄水层之水体.
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将经过换热的地下水通过回灌井把地下水回灌到原来的地下水层.
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As aquifers are drained, more suburbs beyond the basin will ask for it.
而随着地下蓄水层逐渐流干, 大湖盆地外会有越来越多的郊区也提出这样的请求.
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Both the shallow and deep aquifers are highly over-exploited a large area of Hai river basin.
海河平原的的浅层和深层含水层大面积处于严重超采状态.
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All thermal waters in aquifers are medical mineral waters, which is conducive to good health.
所有含水层中的热水都是医疗矿水, 有益于人类的健康.
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Some might still be locked in aquifers and other form . ations beneath the surface.
有些水也许还被锁在蓄水层和其它地表以下的构造中.
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在本次研究的大同盆地,全新世含水层中天然成因的砷破坏了居民安全饮用水的长期供应。
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在对水样进行电导率及Cl-浓度测试的基础上,使用径向收敛流场瞬时注入标准曲线配线法求得试验场地潜水含水层的弥散参数。
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