Prediction of Injection-Induced Cooling using Tracer Test Data in the Hellisheiði Geothermal Field, SW-Iceland Comparison of Numerical and Analytical Modelling Approaches

The Hellisheiði geothermal system is a fracture-controlled geothermal system located in the south part of the Hengill volcanic system in SW-Iceland. The bedrock mainly consists of a sequence of basaltic lavas, hyaloclastites and intrusions. Abundant extensional and transform faults reflect its locat...

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Bibliographic Details
Main Author: Teka Nigussie Gebru 1986-
Other Authors: Háskóli Íslands
Format: Master Thesis
Language:English
Published: 2023
Subjects:
Online Access:http://hdl.handle.net/1946/43321
id ftskemman:oai:skemman.is:1946/43321
record_format openpolar
spelling ftskemman:oai:skemman.is:1946/43321 2024-09-15T18:13:39+00:00 Prediction of Injection-Induced Cooling using Tracer Test Data in the Hellisheiði Geothermal Field, SW-Iceland Comparison of Numerical and Analytical Modelling Approaches Teka Nigussie Gebru 1986- Háskóli Íslands 2023-01 application/pdf http://hdl.handle.net/1946/43321 en eng http://hdl.handle.net/1946/43321 Jarðfræði (námsgrein) Jarðhitarannsóknir Jarðhitakerfi Jarðhiti Thesis Master's 2023 ftskemman 2024-08-14T04:39:51Z The Hellisheiði geothermal system is a fracture-controlled geothermal system located in the south part of the Hengill volcanic system in SW-Iceland. The bedrock mainly consists of a sequence of basaltic lavas, hyaloclastites and intrusions. Abundant extensional and transform faults reflect its location near a triple junction. The objective of this study is to construct a numerical reservoir model of the Hellisheiði geothermal system with a particular focus on reinjection-induced cooling in the Húsmúli subfield. A numerical model is calibrated using natural state temperature profiles, as well as recent tracer data collected in 2019, and is used to predict magnitude and timescale of cooling due to long term reinjection. Using the dual porosity approach, the model is able to achieve a fairly good match to field data for three monitoring wells (HE-31, HE-48, HE-48). The tracer flow in the numerical model constructed underscores the role of the NE oriented fault structures as the main conduits for tracer migration, and the role of transform structures as flow barriers. The model predict an annual temperature decrease of less than 1°C for wells HE-31 and HE-48. On the other hand, although very little tracer appeared in well HE-33 suggesting little risk of injection-induced cooling, the model suggests it may be affected by cooling due to cold water recharge from neighbouring formations. The cooling predictions are compared with those of a simple one-dimensional model (TRINV software). Despite its simple internal structure, TRINV provides greater tracer simulation accuracy. This study supports the importance of reinjection that not only provides pressure support but also helps to counteract colder marginal recharge from surrounding formations. Geothermal Training Program (GRÓ-GTP) Master Thesis Iceland Skemman (Iceland)
institution Open Polar
collection Skemman (Iceland)
op_collection_id ftskemman
language English
topic Jarðfræði (námsgrein)
Jarðhitarannsóknir
Jarðhitakerfi
Jarðhiti
spellingShingle Jarðfræði (námsgrein)
Jarðhitarannsóknir
Jarðhitakerfi
Jarðhiti
Teka Nigussie Gebru 1986-
Prediction of Injection-Induced Cooling using Tracer Test Data in the Hellisheiði Geothermal Field, SW-Iceland Comparison of Numerical and Analytical Modelling Approaches
topic_facet Jarðfræði (námsgrein)
Jarðhitarannsóknir
Jarðhitakerfi
Jarðhiti
description The Hellisheiði geothermal system is a fracture-controlled geothermal system located in the south part of the Hengill volcanic system in SW-Iceland. The bedrock mainly consists of a sequence of basaltic lavas, hyaloclastites and intrusions. Abundant extensional and transform faults reflect its location near a triple junction. The objective of this study is to construct a numerical reservoir model of the Hellisheiði geothermal system with a particular focus on reinjection-induced cooling in the Húsmúli subfield. A numerical model is calibrated using natural state temperature profiles, as well as recent tracer data collected in 2019, and is used to predict magnitude and timescale of cooling due to long term reinjection. Using the dual porosity approach, the model is able to achieve a fairly good match to field data for three monitoring wells (HE-31, HE-48, HE-48). The tracer flow in the numerical model constructed underscores the role of the NE oriented fault structures as the main conduits for tracer migration, and the role of transform structures as flow barriers. The model predict an annual temperature decrease of less than 1°C for wells HE-31 and HE-48. On the other hand, although very little tracer appeared in well HE-33 suggesting little risk of injection-induced cooling, the model suggests it may be affected by cooling due to cold water recharge from neighbouring formations. The cooling predictions are compared with those of a simple one-dimensional model (TRINV software). Despite its simple internal structure, TRINV provides greater tracer simulation accuracy. This study supports the importance of reinjection that not only provides pressure support but also helps to counteract colder marginal recharge from surrounding formations. Geothermal Training Program (GRÓ-GTP)
author2 Háskóli Íslands
format Master Thesis
author Teka Nigussie Gebru 1986-
author_facet Teka Nigussie Gebru 1986-
author_sort Teka Nigussie Gebru 1986-
title Prediction of Injection-Induced Cooling using Tracer Test Data in the Hellisheiði Geothermal Field, SW-Iceland Comparison of Numerical and Analytical Modelling Approaches
title_short Prediction of Injection-Induced Cooling using Tracer Test Data in the Hellisheiði Geothermal Field, SW-Iceland Comparison of Numerical and Analytical Modelling Approaches
title_full Prediction of Injection-Induced Cooling using Tracer Test Data in the Hellisheiði Geothermal Field, SW-Iceland Comparison of Numerical and Analytical Modelling Approaches
title_fullStr Prediction of Injection-Induced Cooling using Tracer Test Data in the Hellisheiði Geothermal Field, SW-Iceland Comparison of Numerical and Analytical Modelling Approaches
title_full_unstemmed Prediction of Injection-Induced Cooling using Tracer Test Data in the Hellisheiði Geothermal Field, SW-Iceland Comparison of Numerical and Analytical Modelling Approaches
title_sort prediction of injection-induced cooling using tracer test data in the hellisheiði geothermal field, sw-iceland comparison of numerical and analytical modelling approaches
publishDate 2023
url http://hdl.handle.net/1946/43321
genre Iceland
genre_facet Iceland
op_relation http://hdl.handle.net/1946/43321
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