Numerical modeling of reinjection and tracer transport in a shallow aquifer, Nesjavellir Geothermal System, Iceland

Abstract Reinjection of excess water from the power production process in the Nesjavellir geothermal field has increased the temperature of shallow groundwaters, posing a risk to cold water wells used for the power plant as well as the ecosystem in Lake Thingvellir. Here, we present a numerical mode...

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Published in:Geothermal Energy
Main Authors: Esteban Gómez-Díaz, Samuel Scott, Thomas Ratouis, Juliet Newson
Format: Article in Journal/Newspaper
Language:English
Published: SpringerOpen 2022
Subjects:
Online Access:https://doi.org/10.1186/s40517-022-00217-3
https://doaj.org/article/a0567dd3b2924a5ebcfbd25922a5ae52
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spelling ftdoajarticles:oai:doaj.org/article:a0567dd3b2924a5ebcfbd25922a5ae52 2023-05-15T16:51:16+02:00 Numerical modeling of reinjection and tracer transport in a shallow aquifer, Nesjavellir Geothermal System, Iceland Esteban Gómez-Díaz Samuel Scott Thomas Ratouis Juliet Newson 2022-04-01T00:00:00Z https://doi.org/10.1186/s40517-022-00217-3 https://doaj.org/article/a0567dd3b2924a5ebcfbd25922a5ae52 EN eng SpringerOpen https://doi.org/10.1186/s40517-022-00217-3 https://doaj.org/toc/2195-9706 doi:10.1186/s40517-022-00217-3 2195-9706 https://doaj.org/article/a0567dd3b2924a5ebcfbd25922a5ae52 Geothermal Energy, Vol 10, Iss 1, Pp 1-28 (2022) Numerical modeling Geothermal reinjection Dual porosity MINC Tracer injection Fluid flow Renewable energy sources TJ807-830 Geology QE1-996.5 article 2022 ftdoajarticles https://doi.org/10.1186/s40517-022-00217-3 2022-12-30T23:22:09Z Abstract Reinjection of excess water from the power production process in the Nesjavellir geothermal field has increased the temperature of shallow groundwaters, posing a risk to cold water wells used for the power plant as well as the ecosystem in Lake Thingvellir. Here, we present a numerical model of fluid flow and heat transport in the shallow reinjection zone to elucidate the flow path of reinjected liquid and the impact of reinjection on the temperature of groundwaters. The permeability structure of the model is based on a 3D geological model of the area. The numerical simulation is calibrated against underground water temperature data measured between 1998 and 2018 and data from a tracer test performed in 2018–2019. The model reproduces the overall temperature field and shows how a high-permeability lava flow together with rift-parallel normal faults act as permeable channels controlling fluid transport. If injection continues, the temperature along the lava flow increases considerably and spreads vertically to much deeper levels, generating a narrow warm zone along the main fault. If shallow injection ceases, temperature drops rapidly at the surface, but decreases slowly around the reinjection zone over 20 years. The numerical model in this study allowed a better characterization of the fracture–matrix interface and the porosity of post-glacial lava flows, contributing to sustainable management of the geothermal resource and the surrounding environment. Article in Journal/Newspaper Iceland Directory of Open Access Journals: DOAJ Articles Nesjavellir ENVELOPE(-21.251,-21.251,64.115,64.115) Geothermal Energy 10 1
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Numerical modeling
Geothermal reinjection
Dual porosity
MINC
Tracer injection
Fluid flow
Renewable energy sources
TJ807-830
Geology
QE1-996.5
spellingShingle Numerical modeling
Geothermal reinjection
Dual porosity
MINC
Tracer injection
Fluid flow
Renewable energy sources
TJ807-830
Geology
QE1-996.5
Esteban Gómez-Díaz
Samuel Scott
Thomas Ratouis
Juliet Newson
Numerical modeling of reinjection and tracer transport in a shallow aquifer, Nesjavellir Geothermal System, Iceland
topic_facet Numerical modeling
Geothermal reinjection
Dual porosity
MINC
Tracer injection
Fluid flow
Renewable energy sources
TJ807-830
Geology
QE1-996.5
description Abstract Reinjection of excess water from the power production process in the Nesjavellir geothermal field has increased the temperature of shallow groundwaters, posing a risk to cold water wells used for the power plant as well as the ecosystem in Lake Thingvellir. Here, we present a numerical model of fluid flow and heat transport in the shallow reinjection zone to elucidate the flow path of reinjected liquid and the impact of reinjection on the temperature of groundwaters. The permeability structure of the model is based on a 3D geological model of the area. The numerical simulation is calibrated against underground water temperature data measured between 1998 and 2018 and data from a tracer test performed in 2018–2019. The model reproduces the overall temperature field and shows how a high-permeability lava flow together with rift-parallel normal faults act as permeable channels controlling fluid transport. If injection continues, the temperature along the lava flow increases considerably and spreads vertically to much deeper levels, generating a narrow warm zone along the main fault. If shallow injection ceases, temperature drops rapidly at the surface, but decreases slowly around the reinjection zone over 20 years. The numerical model in this study allowed a better characterization of the fracture–matrix interface and the porosity of post-glacial lava flows, contributing to sustainable management of the geothermal resource and the surrounding environment.
format Article in Journal/Newspaper
author Esteban Gómez-Díaz
Samuel Scott
Thomas Ratouis
Juliet Newson
author_facet Esteban Gómez-Díaz
Samuel Scott
Thomas Ratouis
Juliet Newson
author_sort Esteban Gómez-Díaz
title Numerical modeling of reinjection and tracer transport in a shallow aquifer, Nesjavellir Geothermal System, Iceland
title_short Numerical modeling of reinjection and tracer transport in a shallow aquifer, Nesjavellir Geothermal System, Iceland
title_full Numerical modeling of reinjection and tracer transport in a shallow aquifer, Nesjavellir Geothermal System, Iceland
title_fullStr Numerical modeling of reinjection and tracer transport in a shallow aquifer, Nesjavellir Geothermal System, Iceland
title_full_unstemmed Numerical modeling of reinjection and tracer transport in a shallow aquifer, Nesjavellir Geothermal System, Iceland
title_sort numerical modeling of reinjection and tracer transport in a shallow aquifer, nesjavellir geothermal system, iceland
publisher SpringerOpen
publishDate 2022
url https://doi.org/10.1186/s40517-022-00217-3
https://doaj.org/article/a0567dd3b2924a5ebcfbd25922a5ae52
long_lat ENVELOPE(-21.251,-21.251,64.115,64.115)
geographic Nesjavellir
geographic_facet Nesjavellir
genre Iceland
genre_facet Iceland
op_source Geothermal Energy, Vol 10, Iss 1, Pp 1-28 (2022)
op_relation https://doi.org/10.1186/s40517-022-00217-3
https://doaj.org/toc/2195-9706
doi:10.1186/s40517-022-00217-3
2195-9706
https://doaj.org/article/a0567dd3b2924a5ebcfbd25922a5ae52
op_doi https://doi.org/10.1186/s40517-022-00217-3
container_title Geothermal Energy
container_volume 10
container_issue 1
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