Titlebook: H2Karst Research in Limestone Hydrogeology; Jacques Mudry,Fran?ois Zwahlen,James W. LaMoreaux Book 2014 The Editor(s) (if applicable) and

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STALE

Aggressive

https://doi.org/10.1007/978-3-319-06139-9Groundwater Flow; H2Karst; Hydrogeology; Karst Aquifer

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Hydraulic Properties of Karst Groundwater and Its Impacts on Large Structures,established but final effects appear abruptly, causing considerable damages or failures. The most common consequences of these impacts are subsidence at the urban areas, along the roads and railways, as well as at the bottom of reservoirs; water seepage from reservoirs; break-in of groundwater under

天真

Inferred Conduit Network Geometry from Geological Evidences and Water-Head in a Fluvio-Karstic Systts and in the host rock are respectively described by the Manning-Strickler equation and Darcy’s law. Constant boundary conditions and hydrodynamic properties are assumed to test the model sensitivity to different network geometry scenarios. The most relevant scenario is selected by comparing calcul

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Oafishness

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Terrace

Distributed Hydrological Modeling and Model Adaption in High Alpine Karst at Regional Scale (Bercht is assumed, that subsurface flow channels and heterogeneous storage effects lead to groundwater redistribution through mountain ranges and influence hydrological processes of neighboring valleys. In a first step, former karst research in the area is evaluated to draw the main subsurface flow direct

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Diagnostic Plots Applied to Well-Tests in Karst Systems,) bi-linear flows within both the karst conduit an the fractured matrix at early times, followed by (2) radial flows within the fractured matrix and (3) finally the contribution of a major karst cavity. The use of diagnostic plots allows the identification of the various flow regimes during pumping