Abstract:Underground excavations usually have a significant impact on hydrogeological runoff. Water seepage affects underground construction and the long-term behaviour of the structure. The flow paths can be altered by underground activity and the spring areas can become infiltration zones. Concerning the healthy massif, permeabilities near a cavity can increase or decrease. The increase in permeability through excavations in an environment of shear stress and associated water inlets, have a lapse, which can lead to p… Show more
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