M. Kracht
Technische Universität Darmstadt
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Zeitschrift Der Deutschen Gesellschaft Fur Geowissenschaften | 2011
K. Bär; D. Arndt; J.-G. Fritsche; Annette E. Götz; M. Kracht; Andreas Hoppe
Within the scope of the research project “3D-modelling of the deep geothermal potentials of Hesse” the deep geothermal potential of the Federal State of Hesse was quantifi ed and assessed in a qualitative analysis. The quantifi cation of the heat stored under ground and the qualitative analysis was done for different geothermal systems. These are hydrothermal and petrothermal systems, as well as fault zones and deep borehole heat exchangers. For the assessment of the deep geothermal potential, knowledge of the geological structure and the geothermal properties of the potential reservoir rocks are indispensable. Therefore, a 3D model of the deep geothermal potential of the Federal State of Hesse (Germany) has been developed (cf. Arndt et al. 2011). Systematic measurements of thermophysical and hydraulic rock properties such as thermal conductivity, heat capacity and permeability of relevant geologic formations have been combined with in-situ temperature measurements, hydrothermal upwelling zones, characteristics of geological faults and were added to the 3D geological structural model. Using a multiple criteria approach, the various rock and reservoir properties were assessed incorporating their relevance for the different geothermal systems to allow the qualitative analysis. Therefore, threshold values for each parameter were defi ned specifying whether the potential is very high, high, medium, low or very low. This method was tested for the one-dimensional case (virtual drilling) and the two-dimensional case (geological-geothermical cross-sections) before being applied to the 3D model. The resulting geothermal model, which incorporates the quantifi cation and the qualitative analysis, is an important tool, which can be used at an early stage of the planning phase for the design of geothermal power plants. Furthermore, it allows quantifi cation of the deep geothermal potential and is intended to be an instrument for public information. Schlusselworter: Geothermie, geothermisches Potenzial, thermophysikalische Gesteinseigenschaften, hydraulische Kennwerte, geologisches 3D-Modell, Oberrheingraben, Hessen, Deutschland, GOCAD
Archive | 2011
K. Bär; D. Arndt; J.-G. Fritsche; M. Kracht; Andreas Hoppe
Energy Procedia | 2015
J. Freymark; Judith Sippel; Magdalena Scheck-Wenderoth; K. Bär; M. Stiller; M. Kracht; J.-G. Fritsche
Tectonophysics | 2017
J. Freymark; Judith Sippel; Magdalena Scheck-Wenderoth; K. Bär; M. Stiller; J.-G. Fritsche; M. Kracht
Archive | 2017
J. Freymark; Judith Sippel; Magdalena Scheck-Wenderoth; K. Bär; M. Stiller; J.-G. Fritsche; M. Kracht
Archive | 2017
J. Freymark; Judith Sippel; M. Cacace; Magdalena Scheck-Wenderoth; K. Bär; M. Ziegler; M. Stiller; J.-G. Fritsche; M. Kracht
Archive | 2017
J. Freymark; Judith Sippel; Magdalena Scheck-Wenderoth; K. Bär; M. Stiller; J.-G. Fritsche; M. Kracht
Archive | 2016
J. Freymark; Judith Sippel; Magdalena Scheck-Wenderoth; K. Bär; M. Stiller; J.-G. Fritsche; M. Kracht
Archive | 2016
J. Freymark; Judith Sippel; Magdalena Scheck-Wenderoth; K. Bär; M. Stiller; J.-G. Fritsche; M. Kracht
Grundwasser | 2016
J.-G. Fritsche; Jan Brodsky; Heiner Heggemann; Michaela Hoffmann; Martin Hottenrott; M. Kracht; Thomas Reischmann; Fred Rosenberg; Inga Schlösser-Kluger