Crustal-Scale Thermal Models: Revisiting the Influence of Deep Boundary
Conditions
- Denise Degen
, - Karen Veroy,
- Magdalena Scheck-Wenderoth,
- Florian Wellmann

Denise Degen

RWTH Aachen University, RWTH Aachen University
Corresponding Author:denise.degen@cgre.rwth-aachen.de
Author ProfileKaren Veroy
Eindhoven University of Technology, Eindhoven University of Technology
Author ProfileMagdalena Scheck-Wenderoth
Helmholtz Centre Potsdam, GFZ German Research Science for Geosciences, Helmholtz Centre Potsdam, GFZ German Research Science for Geosciences
Author ProfileFlorian Wellmann

RWTH Aachen University, RWTH Aachen University
Author ProfileAbstract
The societal importance of geothermal energy is significantly increasing
because of its low carbon-dioxide footprint. However, geothermal
exploration is also subject to high risks. For a better assessment of
these risks, extensiveparameter studies are required that improve our
understanding of the subsurface. This yields computationally demanding
analyses. Often this is compensated by constructing models with a low
vertical extent. In this paper, we demonstrate that this leads to
entirely boundary-dominated and hence uninformative models. We
demonstrate the indispensable requirement to construct models with a
large vertical extent to obtain informative models with respect to the
model parameters. For this quantitative investigation, global
sensitivity studies are essential since they also consider parameter
correlations. To compensate for the computationally demanding nature of
the analyses, we employ a physics-based machine learning approach,
namely the reduced basis method, instead of reducing the physical
dimensionality of the model. The reduced basis method yields a
significant cost reduction while preserving the physics and a high
accuracy, thus providing a more efficient alternative to considering,
for instance, a lower vertical extent. The reduction of the mathematical
instead of physical space leads to less restrictive models and, hence,
maintains the model prediction capabilities. We use this combination of
methods for a detailed investigation of the influence of model boundary
settings in typical regional-scale geothermal simulations and highlight
potential problems.