Geophysical Site Characterization and monitoring of CO2 mineralization in Basaltic Complexes, Helguvik, Iceland

In a pilot project (DemoUpStorage) in Helguvik, Iceland, CO2 is injected into basaltic strata using seawater instead of freshwater for CO2 dissolution. The aim is to obtain permanent storage of the CO2 by mineral carbonation. We aim to observe the precipitation of Mg and Fe carbonates in the porosit...

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Main Authors: Junker, Jonas Simon, Obermann, Anne, id_orcid:0 000-0001-6933-6301, Zappone, Alba Simona, id_orcid:0 000-0003-0965-7271, Maurer, Hansruedi, Wiemer, Stefan, id_orcid:0 000-0002-4919-3283
Format: Conference Object
Language:English
Published: Copernicus 2024
Subjects:
Online Access:https://hdl.handle.net/20.500.11850/715662
https://doi.org/10.3929/ethz-b-000715662
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author Junker, Jonas Simon
Obermann, Anne
id_orcid:0 000-0001-6933-6301
Zappone, Alba Simona
id_orcid:0 000-0003-0965-7271
Maurer, Hansruedi
Wiemer, Stefan
id_orcid:0 000-0002-4919-3283
author_facet Junker, Jonas Simon
Obermann, Anne
id_orcid:0 000-0001-6933-6301
Zappone, Alba Simona
id_orcid:0 000-0003-0965-7271
Maurer, Hansruedi
Wiemer, Stefan
id_orcid:0 000-0002-4919-3283
author_sort Junker, Jonas Simon
collection ETH Zürich Research Collection
description In a pilot project (DemoUpStorage) in Helguvik, Iceland, CO2 is injected into basaltic strata using seawater instead of freshwater for CO2 dissolution. The aim is to obtain permanent storage of the CO2 by mineral carbonation. We aim to observe the precipitation of Mg and Fe carbonates in the porosity of the reservoir at depth. Additional to geochemical observations, we use geophysical methods (ERT, seismics) to monitor the mineralization process. Here, we present the overall project, the geophysical characterization of the site and the first time-lapse monitoring results. We performed a cross-hole seismic traveltime tomography and single-hole electrical resistivity (ERT) measurements to characterize the study site in the target depth of 150m to 400m and to record a geophysical baseline for the time-lapse measurements. The seismic and geoelectric data are in good agreement, highlighting multiple basaltic layers of tens of meters in thickness with sedimentary interlayers. With the CO2 injection starting in early 2024, we will also show the first results from the (daily) time-lapse ERT surveys.
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spelling ftethz:oai:www.research-collection.ethz.ch:20.500.11850/715662 2025-03-02T15:30:54+00:00 Geophysical Site Characterization and monitoring of CO2 mineralization in Basaltic Complexes, Helguvik, Iceland Junker, Jonas Simon Obermann, Anne id_orcid:0 000-0001-6933-6301 Zappone, Alba Simona id_orcid:0 000-0003-0965-7271 Maurer, Hansruedi Wiemer, Stefan id_orcid:0 000-0002-4919-3283 2024-04-16 application/application/pdf https://hdl.handle.net/20.500.11850/715662 https://doi.org/10.3929/ethz-b-000715662 en eng Copernicus info:eu-repo/semantics/altIdentifier/doi/10.5194/egusphere-egu24-9061 http://hdl.handle.net/20.500.11850/715662 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International EGUsphere info:eu-repo/semantics/conferenceObject info:eu-repo/semantics/updatedVersion 2024 ftethz https://doi.org/20.500.11850/71566210.3929/ethz-b-00071566210.5194/egusphere-egu24-9061 2025-02-11T02:44:00Z In a pilot project (DemoUpStorage) in Helguvik, Iceland, CO2 is injected into basaltic strata using seawater instead of freshwater for CO2 dissolution. The aim is to obtain permanent storage of the CO2 by mineral carbonation. We aim to observe the precipitation of Mg and Fe carbonates in the porosity of the reservoir at depth. Additional to geochemical observations, we use geophysical methods (ERT, seismics) to monitor the mineralization process. Here, we present the overall project, the geophysical characterization of the site and the first time-lapse monitoring results. We performed a cross-hole seismic traveltime tomography and single-hole electrical resistivity (ERT) measurements to characterize the study site in the target depth of 150m to 400m and to record a geophysical baseline for the time-lapse measurements. The seismic and geoelectric data are in good agreement, highlighting multiple basaltic layers of tens of meters in thickness with sedimentary interlayers. With the CO2 injection starting in early 2024, we will also show the first results from the (daily) time-lapse ERT surveys. Conference Object Iceland ETH Zürich Research Collection
spellingShingle Junker, Jonas Simon
Obermann, Anne
id_orcid:0 000-0001-6933-6301
Zappone, Alba Simona
id_orcid:0 000-0003-0965-7271
Maurer, Hansruedi
Wiemer, Stefan
id_orcid:0 000-0002-4919-3283
Geophysical Site Characterization and monitoring of CO2 mineralization in Basaltic Complexes, Helguvik, Iceland
title Geophysical Site Characterization and monitoring of CO2 mineralization in Basaltic Complexes, Helguvik, Iceland
title_full Geophysical Site Characterization and monitoring of CO2 mineralization in Basaltic Complexes, Helguvik, Iceland
title_fullStr Geophysical Site Characterization and monitoring of CO2 mineralization in Basaltic Complexes, Helguvik, Iceland
title_full_unstemmed Geophysical Site Characterization and monitoring of CO2 mineralization in Basaltic Complexes, Helguvik, Iceland
title_short Geophysical Site Characterization and monitoring of CO2 mineralization in Basaltic Complexes, Helguvik, Iceland
title_sort geophysical site characterization and monitoring of co2 mineralization in basaltic complexes, helguvik, iceland
url https://hdl.handle.net/20.500.11850/715662
https://doi.org/10.3929/ethz-b-000715662