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Geophysical methods help to assess potential groundwater extraction sites

机译:地球物理方法有助于评估潜在的地下水开采地点

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摘要

Complex geology in glacial terrain makes groundwater exploration challenging for water supply companies. Abrupt lateral changes of geological conditions, for example, raise the risk of unsuccessful exploration drilling. At some locations, local water supply companies experience a?large number of dry wells, raising the need for better exploration approaches. The use of geophysical techniques enables the detection and characterization of subsurface structures in terms of aquifers and aquitards.We present two examples in which seismic and resistivity methods are combined for subsurface characterization. A?thrust structure is detected in the Varde study area in Denmark and a?channel structure is mapped in the Hamburg-Sülldorf study area in Germany. The different imaging characteristics of seismic P? and S?waves are demonstrated. The combination of seismic and resistivity methods enables delineating groundwater-bearing and groundwater-barrier layers down to a?depth of 150?m.
机译:冰川地形的复杂地质使地下水勘探对供水公司来说具有挑战性。例如,地质条件的突然横向变化会增加勘探钻探失败的风险。在一些地方,当地供水公司经历了大量的干井,这增加了对更好的勘探方法的需求。使用地球物理技术可以探测和表征含水层和滞水层的地下结构。我们提出了两个例子,其中地震和电阻率方法相结合进行地下表征。在丹麦Varde研究区探测到逆冲结构,在德国Hamburg-Sülldorf研究区绘制了通道结构图。地震P?并演示了 S?波。地震法和电阻率法相结合,可以划定地下含水层和地下水屏障层,深度可达150米。

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