Introduction – Motivation
This pilot project aims at characterizing the geothermal heat-flux distribution in the Canton of Aargau to aid in the estimation of its geothermal potential. In Northern Switzerland, surface heat fluxes can reach up to 140 mW m-2, significantly higher than the Swiss average (Medici and Rybach, 1995). This may be caused by advective heat transport along Paleozoic faults in the crystalline basement. These are most likely normal faults bounding a major Permo-Carboniferous trough in the northern part of the Canton of Aargau (see Fig. 1). However, different explanations for the high surface heat fluxes exist, for instance, that two topographically driven flow regimes, southward from the Black Forest, and northward through the Mesozoic Molasse, meet in the project area and create a heat-flow anomaly as a consequence of upwelling. This formed surface-heat-flow anomaly would not be bound to fluids ascending along faults in the crystalline basement. Part of this project is to test these hypotheses, concerning different groundwater flow systems causing a heat-flow anomaly in the Canton Aargau (Figure 1) by using numerical modeling.
The project’s main objective is to produce model-based maps of the deep heat flow in the area as a reference for decision makers for potential future geothermal projects. These maps will comprise average heat-flow values at a depth of several kilometers, as well as their uncertainty. This is to be achieved by combining (geometrical) uncertainty of geological 3D models with (parametric) uncertainty of numerical heat-transport models in a Bayesian framework (de la Varga et al., 2016; Schneeberger et al., 2017; Wellmann and Caumon, 2018). Modelling and uncertainty evaluation will be integrated in an adaptive workflow which, in future, may be used for similar studies in other regions.
Figure 1: Our map of the project area in the Canton Aargau. Permo-Carboniferous troughs are outlined based on Leu (2008) and Abdelfettah (2014). The heat-flow contours are based on Medici and Rybach (1995).
An integrative, adaptive, and reproducible workflow is at the core of this project, and comprises four major steps as depicted in Figure 2.
The initial step “Data preparation” comprises a multitude of tasks such as homogenization and standardization of data based on Strasky et al. (2016), who developed a lithostratigraphic lexicon of Switzerland, with the aim of harmonizing the existing lithostratigraphic nomenclature.
In the chosen method of handling legacy data, an iteratively built geological model does not necessarily have to fit single data points, but it is also used to test data. This approach, based on Corbel and Wellmann (2015), enables a modeler to distinguish between (model-)consistent data and (for the model) unusable data.
Steps Two and Three, namely “Geological Modelling” and “Reservoir Simulation”, are an iterative process, where a suite of different geological model hypotheses is evaluated by numerical simulation of heat and mass transport in the geological model. The final result will likely be an ensemble of conditionally probable heat-transport models of the study area.
Figure 2: Simplified depiction of the intended project workflow, based on four major steps.
For modeling the spatial geometry of geological structures and lithologies, we test an implicit potential-field approach (Lajaunie et al., 1997; Wellmann and Caumon, 2018; de la Varga et al., 2019). In Figure 3, the two input data types for the model are shown: interface points (colored circles) and orientation points (black arrow heads), based on seismic interpretations by Naef and Madritsch (2014). The resulting simplified, discretized 2D model of a Permo-Carboniferous trough is shown as colors. Existing geological models, such as GeoMol (GeoMol Team, 2015), will be considered and merged with the model hypotheses in the presented modeling workflow.
Figure 3: Simplified 2D geological model based on the interpretation of seismic line 11-NS-06 by Naef and Madritsch (2014).
The results of the geological modelling process, i.e. the geological structures, are transferred to a framework for simulating fluid mass and heat transfer (MOOSE framework; Gaston et al., 2009). It provides a porous flow module comprising all necessary governing equations for simulating fluid mass and heat transport in a geothermal reservoir system (e.g. Figure 4).
Calibrated simulation results will be merged in an ensemble comprising conditioned model realizations. This ensemble is then used for generating the aforementioned heat-flow maps with associated uncertainty.
Figure 4: Preliminary, purely conductive temperature field simulation of the modeled geological cross-section in Figure 3. The shape of the graben system can be inferred, due to the different thermal conductivities of the lithological units.
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