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Type: Article × Subject: Hydraulic properties ×

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    Geothermal potential of the Buntsandstein and Keuper aquifers in NE Bavaria with a focus on deep thermal aquifer storage
    (Berlin ; Heidelberg : Springer, 2019-9-26) Kunkel, Cindy; Agemar, Thorsten; Stober, Ingrid
    Intermediate and deep geothermal resources of Germany are limited to medium and low enthalpy resources. These resources are predominantly used for balneological applications, space and district heating and for power production at nine separate sites. This study focuses on confined aquifers in northeast Bavaria, which can be used for balneology as well as energy storage. Data from pumping tests and production data were interpreted to map the hydraulic conductivity of the main Keuper and Buntsandstein aquifers with a large spatial distribution for geothermal applications deeper than 100 m. Furthermore, temperature estimates as well as the depth of the two aquifers (Keuper 100 to 650 m, Buntsandstein 100 to 1400 m) are incorporated. The results will be visualized in the form of spatial distribution maps of the hydraulic conductivity and temperature, and will be integrated into the geothermal information system GeotIS (https://www.geotis.de). Altogether, about 80% of all 243 sampling sites show hydraulic conductivity values sufficient for geothermal energy utilization. For the Keuper aquifer, even 90% of all 155 sampling sites show transmissivities sufficient for geothermal energy utilization. However, these maps do not replace a feasibility study for specific geothermal projects because detailed geological site assessment is essential when planning a subsurface geothermal system.
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    Hydraulic properties at the North Sea island of Borkum derived from joint inversion of magnetic resonance and electrical resistivity soundings
    (Munich : EGU, 2012) Günther, T.; Müller-Petke, M.
    For reliably predicting the impact of climate changes on salt/freshwater systems below barrier islands, a long-term hydraulic modelling is inevitable. As input we need the parameters porosity, salinity and hydraulic conductivity at the catchment scale, preferably non-invasively acquired with geophysical methods. We present a methodology to retrieve the searched parameters and a lithological interpretation by the joint analysis of magnetic resonance soundings (MRS) and vertical electric soundings (VES). Both data sets are jointly inverted for resistivity, water content and decay time using a joint inversion scheme. Coupling is accomplished by common layer thicknesses. We show the results of three soundings measured on the eastern part of the North Sea island of Borkum. Pumping test data is used to calibrate the petrophysical relationship for the local conditions in order to estimate permeability from nuclear magnetic resonance (NMR) data. Salinity is retrieved from water content and resistivity using a modified Archie equation calibrated by local samples. As a result we are able to predict porosity, salinity and hydraulic conductivities of the aquifers, including their uncertainties. The joint inversion significantly improves the reliability of the results. Verification is given by comparison with a borehole. A sounding in the flooding area demonstrates that only the combined inversion provides a correct subsurface model. Thanks to the joint application, we are able to distinguish fluid conductivity from lithology and provide reliable hydraulic parameters as shown by uncertainty analysis. These findings can finally be used to build groundwater flow models for simulating climate changes. This includes the improved geometry and lithological attribution, and also the parameters and their uncertainties. © Author(s) 2012.