Titlebook: Hydrogeology of Crystalline Rocks; Ingrid Stober,Kurt Bucher Book 2000 Springer Science+Business Media Dordrecht 2000 Geoinformationssyste

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978-90-481-5368-8Springer Science+Business Media Dordrecht 2000

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Hydraulic Properties of the Upper Continental Crust: data from the Urach 3 geothermal wellved solids (TDS) occupies the fracture pore space at depth. The basement can be best described as a homogeneous, isotropic aquifer and this characteristic hydraulic behavior persists to at least several hundred meters around the borehole. No evidence for hydraulic infiltration or the existence of im

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The Role of Water-Conducting Features in the Swiss Concept for the Disposal of High-Level Radioactivon and radioactive decay/ingrowth. Due to the diversity of the types of water-conducting features and of the small-scale geometric parameters, six model cases were considered that spanned the range of geometric parameter uncertainty. Calculated radiological doses are relatively insensitive to variat

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The Scaling of Hydraulic Properties in Granitic Rocks and (2) the presence of transmissive fractures outside the well screen that allow additional discharge to the borehole. More data are needed to verify whether the relationship found for fractured crystalline carbonates is also valid for granitic rocks because of the larger local variations in hydra