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1)  pouring water aquifers
突水含水层
1.
Took 38 water samples from four of the main pouring water aquifers in the mining area in northern Anhui such as Linhuan Mine, Haizi Mine and so on, analyzed the content of the radioactive isotope tritium, and drew the content of tritium isoline figures about the fourth aquifer, the Taiyuan limestone aquifer and the Ordovician limestone aquifer.
在皖北矿区的临涣、海孜等矿对4个主要突水含水层采取了38个水样,做了放射性同位素氚含量分析,绘制了四含水、太灰水和奥灰水氚含量等值线图。
2)  water inrush through fault
断层突水
1.
Numerical simulation of the analysis of possibility of water inrush through fault;
断层突水风险的数值模拟
2.
Solid-liquid coupling study on water inrush through faults in coal mining above confined aquifer;
承压水上采煤断层突水的固流耦合研究
3)  water inrush from red bed
红层突水
4)  the 7th water bearing bed (Qihan) water inrush
七含涌(突)水
5)  saline aquifer
咸水含水层
1.
The enormous saline aquifers deeply buried in the sedimentary basins are saturated with high concentration dissolved solids,which make groundwater unsuitable to any large-scale exploitation.
沉积盆地地下深部存在体积巨大的咸水含水层,咸水不宜开发利用,可用来储存大量的CO2。
6)  unconfined aquifer
潜水含水层
1.
Vulnerability assessment for unconfined aquifer in Guanzhong basin;
关中盆地潜水含水层脆弱性评价
2.
Calculation of typical unconfined aquifer seepage to a shallow lake with gentle slope bottom;
典型潜水含水层通过缓坡湖底的渗流量计算
3.
According to the framework of ModIME and experience in practice,problems existing in simulating unconfined aquifer are pointed out herein to avoid simulation deviation caused by the software itself.
根据ModIME的结构和实际使用经验 ,指出该软件在模拟潜水含水层时存在的问题 ,从而避免因软件本身产生不必要的模拟结果偏差。
补充资料:含水层
      见地下水。
  

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