AbstractThe goal of this study is to quantify the influences of upper hydraulic and temperature boundary conditions on temperatures as calculated by 3D numerical simulations of coupled fluid-and-heat transport for the subsurface of Berlin. Both, the underlying structural model, as well as the sensitivity analysis are data-driven. The results show that the subsurface thermal field is strongly influenced by hydraulic and thermal boundary conditions. Findings of this study suggest that in the model area conductive heat transport processes are able to compensate the influence of advection by pressure gradients. Also, anthropogenic influences on the subsurface thermal field could be quantified
The Upper Rhine Graben and its northern prolongation, the Hessian depression, were formed as part of...
The extensive data sets obtained by the KTB drilling project (lithological and structural informatio...
Shallow subsurface temperatures are influenced by various processes. In particular, the thermal envi...
AbstractThe goal of this study is to quantify the influences of upper hydraulic and temperature boun...
AbstractThe objective of this study is to analyze the influence of geological structure and paramete...
A successful utilization of deep geothermal resources requires accurate predictions about the reserv...
Knowing the thermal and hydraulic conditions below major urban centers is of increasing importance i...
In the context of the provision of clean renewable energy, the utilization of the subsurface of urba...
A successful utilization of deep geothermal resources requires accurate predictions about the distri...
The Upper Rhine Graben (URG) is one of the regions in Germany with promising potentials for deep geo...
AbstractA lithosphere scale geological model has been used to determine the surface heat flow compon...
High-resolution depth-oriented temperature measurements havebeen introduced to investigate a groundw...
The Upper Rhine Graben and its prolongation, the Hessian depression, were formed as part of the Euro...
AbstractWe present a seismic- and 3D-gravity-constrained lithospheric-scale 3D structural model of H...
The Upper Rhine Graben (URG) is an active rift with a high geothermal potential. Despite being a wel...
The Upper Rhine Graben and its northern prolongation, the Hessian depression, were formed as part of...
The extensive data sets obtained by the KTB drilling project (lithological and structural informatio...
Shallow subsurface temperatures are influenced by various processes. In particular, the thermal envi...
AbstractThe goal of this study is to quantify the influences of upper hydraulic and temperature boun...
AbstractThe objective of this study is to analyze the influence of geological structure and paramete...
A successful utilization of deep geothermal resources requires accurate predictions about the reserv...
Knowing the thermal and hydraulic conditions below major urban centers is of increasing importance i...
In the context of the provision of clean renewable energy, the utilization of the subsurface of urba...
A successful utilization of deep geothermal resources requires accurate predictions about the distri...
The Upper Rhine Graben (URG) is one of the regions in Germany with promising potentials for deep geo...
AbstractA lithosphere scale geological model has been used to determine the surface heat flow compon...
High-resolution depth-oriented temperature measurements havebeen introduced to investigate a groundw...
The Upper Rhine Graben and its prolongation, the Hessian depression, were formed as part of the Euro...
AbstractWe present a seismic- and 3D-gravity-constrained lithospheric-scale 3D structural model of H...
The Upper Rhine Graben (URG) is an active rift with a high geothermal potential. Despite being a wel...
The Upper Rhine Graben and its northern prolongation, the Hessian depression, were formed as part of...
The extensive data sets obtained by the KTB drilling project (lithological and structural informatio...
Shallow subsurface temperatures are influenced by various processes. In particular, the thermal envi...