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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MDPI AG
2019-05-01
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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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format | Article |
id | doaj.art-b14168e9936746f58a67588da1279d87 |
institution | Directory Open Access Journal |
issn | 1996-1073 |
language | English |
last_indexed | 2024-04-13T00:25:57Z |
publishDate | 2019-05-01 |
publisher | MDPI AG |
record_format | Article |
series | Energies |
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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