Ground water flow in fractured hard rock based on field data from the Sudety Mts., SW Poland

机译：基于来自波兰西南部Sudety山的现场数据，裂缝性硬岩中的地下水流

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Results of three years' observation on groundwater flow from an abandoned mine adit (gallery) in a fractured metamorphic formation in the Sudety Mts. are reported in this paper. The flow characteristic is discussed together with the results of infiltration measurements and those of water level fluctuation and of total flow in a mountainous river. Hydraulic description of weathering cover and of fracture system is given. Low-rate vertical flow in the clay-rich weathering zone is associated with relatively fast flow in the hard rock fracture system. The ground water residence time in both contrasting layers are discussed.

机译：Sudety山断裂变质地层中废弃的矿井（画廊）的地下水流三年观测结果。在本文中进行了报道。讨论了流量特征以及山地河流的入渗测量结果，水位波动和总流量的结果。给出了风化覆盖层和断裂系统的水力描述。富含粘土的风化带中的低速垂直流与硬岩压裂系统中的相对快的流有关。讨论了两个对比层中的地下水停留时间。

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《New Approaches Characterizing Groundwater Flow》|2001年|p.1069-1072|共4页
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S. Stasko; R. Tarka;
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Ground water flow in fractured hard rock based on field data from the Sudety Mts., SW Poland

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