The Effects of Regional Fluid Flow on Deep Temperatures (Hesse, Germany)

A successful utilization of deep geothermal resources requires accurate predictions about the distribution of reservoir temperature as well as of the hydraulic processes exerting a direct influence on the productivity of geothermal reservoirs. The aim of this study was to investigate and quantify th...

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Main Authors: Nora Koltzer, Magdalena Scheck-Wenderoth, Judith Bott, Mauro Cacace, Maximilian Frick, Ingo Sass, Johann-Gerhard Fritsche, Kristian Bär
Format: Article
Language:English
Published: MDPI AG 2019-05-01
Series:Energies
Subjects:
Online Access:https://www.mdpi.com/1996-1073/12/11/2081
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author Nora Koltzer
Magdalena Scheck-Wenderoth
Judith Bott
Mauro Cacace
Maximilian Frick
Ingo Sass
Johann-Gerhard Fritsche
Kristian Bär
author_facet Nora Koltzer
Magdalena Scheck-Wenderoth
Judith Bott
Mauro Cacace
Maximilian Frick
Ingo Sass
Johann-Gerhard Fritsche
Kristian Bär
author_sort Nora Koltzer
collection DOAJ
description A successful utilization of deep geothermal resources requires accurate predictions about the distribution of reservoir temperature as well as of the hydraulic processes exerting a direct influence on the productivity of geothermal reservoirs. The aim of this study was to investigate and quantify the influence that regional thermo-hydraulic processes have on the geothermal configuration of potential reservoirs in the German Federal State of Hesse. Specifically, we have addressed the question of how the regional thermal and hydraulic configuration influence the local hydro-thermal reservoir conditions. Therefore, a 3D structural model of Hesse was used as a basis for purely hydraulic, purely thermal and coupled 3D thermo-hydraulic simulations of the deep fluid flow and heat transport. As a result of our numerical simulations, Hesse can be differentiated into sub-areas differing in terms of the dominating heat transport process. In a final attempt to quantify the robustness and reliability of the modelling results, the modelling outcomes were analyzed by comparing them to available subsurface temperature, hydraulic and hydrochemical data.
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spelling doaj.art-b14168e9936746f58a67588da1279d872022-12-22T03:10:37ZengMDPI AGEnergies1996-10732019-05-011211208110.3390/en12112081en12112081The Effects of Regional Fluid Flow on Deep Temperatures (Hesse, Germany)Nora Koltzer0Magdalena Scheck-Wenderoth1Judith Bott2Mauro Cacace3Maximilian Frick4Ingo Sass5Johann-Gerhard Fritsche6Kristian Bär7Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, GermanyHelmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, GermanyHelmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, GermanyHelmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, GermanyHelmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, GermanyInstitute of Applied Geosciences, TU Darmstadt, 64287 Darmstadt, GermanyHessian Agency for Nature Conservation, Environment and Geology (HLNUG), 65203 Wiesbaden, GermanyInstitute of Applied Geosciences, TU Darmstadt, 64287 Darmstadt, GermanyA successful utilization of deep geothermal resources requires accurate predictions about the distribution of reservoir temperature as well as of the hydraulic processes exerting a direct influence on the productivity of geothermal reservoirs. The aim of this study was to investigate and quantify the influence that regional thermo-hydraulic processes have on the geothermal configuration of potential reservoirs in the German Federal State of Hesse. Specifically, we have addressed the question of how the regional thermal and hydraulic configuration influence the local hydro-thermal reservoir conditions. Therefore, a 3D structural model of Hesse was used as a basis for purely hydraulic, purely thermal and coupled 3D thermo-hydraulic simulations of the deep fluid flow and heat transport. As a result of our numerical simulations, Hesse can be differentiated into sub-areas differing in terms of the dominating heat transport process. In a final attempt to quantify the robustness and reliability of the modelling results, the modelling outcomes were analyzed by comparing them to available subsurface temperature, hydraulic and hydrochemical data.https://www.mdpi.com/1996-1073/12/11/2081thermo-hydraulic processesthermal fieldUpper Rhine Grabendeep fluid flowHesse3D numerical modelHessian DepressionVogelsberg
spellingShingle Nora Koltzer
Magdalena Scheck-Wenderoth
Judith Bott
Mauro Cacace
Maximilian Frick
Ingo Sass
Johann-Gerhard Fritsche
Kristian Bär
The Effects of Regional Fluid Flow on Deep Temperatures (Hesse, Germany)
Energies
thermo-hydraulic processes
thermal field
Upper Rhine Graben
deep fluid flow
Hesse
3D numerical model
Hessian Depression
Vogelsberg
title The Effects of Regional Fluid Flow on Deep Temperatures (Hesse, Germany)
title_full The Effects of Regional Fluid Flow on Deep Temperatures (Hesse, Germany)
title_fullStr The Effects of Regional Fluid Flow on Deep Temperatures (Hesse, Germany)
title_full_unstemmed The Effects of Regional Fluid Flow on Deep Temperatures (Hesse, Germany)
title_short The Effects of Regional Fluid Flow on Deep Temperatures (Hesse, Germany)
title_sort effects of regional fluid flow on deep temperatures hesse germany
topic thermo-hydraulic processes
thermal field
Upper Rhine Graben
deep fluid flow
Hesse
3D numerical model
Hessian Depression
Vogelsberg
url https://www.mdpi.com/1996-1073/12/11/2081
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