Journal
GRUNDWASSER
Volume 14, Issue 2, Pages 127-137Publisher
SPRINGER HEIDELBERG
DOI: 10.1007/s00767-009-0103-3
Keywords
Upper Rhine Graben; Hydrogeothermal resources; Hydraulic conductivity; Hauptrogenstein; Oberer Muschelkalk; Buntsandstein
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The project entitled aEurozDevelopment of an Internet Based Geothermal System for Germany includes the design of a geothermal information system for the deep hydrogeothermal resources of Germany. For the first time, hydraulic data from the entire Upper Rhine Graben in Baden-Wurttemberg and France were collected and interpreted. They give hydraulic conductivities in the geothermal reservoirs of the Hauptrogenstein, Oberer Muschelkalk and Buntsandstein. The mean value of the Hauptrogenstein south of Freiburg is T/H = 1,8 center dot 10(-6) m/s, and the Oberer Muschelkalk average is T/H = 2,0 center dot 10(-6) m/s. For the Buntsandstein, the hydraulic conductivity is T/H > 2,4 center dot 10(-7) m/s. Estimated hydraulic conductivities derived from productivity indices and permeability data are used for further comparative considerations.
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