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  • 1
    Online Resource
    Online Resource
    Geothermal Energy : from Theoretical Models to Exploration and Development (2021)
    Cham : Springer International Publishing | Cham : Imprint: Springer
    Details Availability
    Keywords: Environmental sciences. ; Renewable energy resources. ; Energy systems. ; Lehrbuch ; Geothermik ; Geothermische Energie ; Geothermisches Kraftwerk ; Erdwärmesonde ; Hydrothermalquelle ; Thermalwasser ; Hot-dry-rock-Verfahren ; Tiefengeothermie ; Tiefe geothermische Energie ; Tiefenwasser
    Description / Table of Contents: Chapter 1: Thermal Structure of The Earth -- Chapter 2: History of Geothermal Energy Use -- Chapter 3: Geothermal Energy Resources -- Chapter 4: Uses of Geothermal Energy -- Chapter 5: Geothermal Potential Perspectives Final -- Chapter 6: Geothermal Probes Final -- Chapter 7: Groundwater Wells -- Chapter 8: Hydrothermal Systems -- Chapter 9: EGS -- Chapter 10: High-Enthalpy Geothermal Systems -- Chapter 11: Environmental Issues -- Chapter 12: Drilling Techniques -- Chapter 13: Geophysical Methods -- Chapter 14: Hydraulic Tests -- Chapter 15: Hydrochemistry -- Chapter 16: References
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource(X, 390 p. 181 illus., 158 illus. in color.)
    Edition: 2nd ed. 2021
    ISBN: 9783030716851
    Series Statement: Springer eBook Collection
    URL: https://doi.org/10.1007/978-3-030-71685-1
    DOI: 10.1007/978-3-030-71685-1
    Language: English
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  • 2
    Electronic Resource
    Electronic Resource
    Permeability distribution in the Quaternary of the Upper Rhine glacio-fluvial aquifer (1997)
    Oxford, UK : Blackwell Science Ltd
    Terra nova 9 (1997), S. 0 
    Details
    ISSN: 1365-3121
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: An extraordinarily large and geographically extensive 3D dataset has allowed us to relate permeability to detailed geological features. Permeability data derived from several thousand pumptests in Quaternary sediments (thickness 〈 120 m) of the Upper Rhine valley vary from K= 4.5 × 10−7 m s−1 to K= 2.7 × 10−1 m s−1. The geometric mean of the data is K= 2.25 × 10−3 m s−1. The permeability distribution maps for four different stratigraphic levels show that the highest values are found in sections beneath recent and historic fluvial systems. Fossil fans of small rivers from the Black Forest can be identified in the Rhine valley on the basis of the permeability pattern. The average hydraulic conductivity decreases S–N along the flow direction which corresponds to a decrease in grain-size of the fluvial sediments.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1046/j.1365-3121.1997.d01-16.x
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