Geochemical modeling of CO2 storage in saline aquifers: examples from Ketzin, In Salah and Snohvit storage sites

Geochemical modeling is an interesting tool to assess the geochemical behavior of CO2 in the saline aquifer, including its dissolution in the brine and its interactions with minerals. The Pitzer interaction model is rarely used for simulating CO2 geochemical behavior in saline aquifers despite the f...

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Main Author: Tremosa, Joachim
Other Authors: Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)
Format: Conference Object
Language:English
Published: HAL CCSD 2013
Subjects:
Online Access:https://hal-brgm.archives-ouvertes.fr/hal-00829892
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spelling ftunivnantes:oai:HAL:hal-00829892v1 2023-05-15T18:20:13+02:00 Geochemical modeling of CO2 storage in saline aquifers: examples from Ketzin, In Salah and Snohvit storage sites Tremosa, Joachim Bureau de Recherches Géologiques et Minières (BRGM) (BRGM) Trondheim, Norway 2013-06-10 https://hal-brgm.archives-ouvertes.fr/hal-00829892 en eng HAL CCSD hal-00829892 https://hal-brgm.archives-ouvertes.fr/hal-00829892 IEAGHG Combined Modelling and Risk Management Network Meeting https://hal-brgm.archives-ouvertes.fr/hal-00829892 IEAGHG Combined Modelling and Risk Management Network Meeting, Jun 2013, Trondheim, Norway CO2 storage geochemical modeling high salinity Pitzer dawsonite [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/conferenceObject Conference papers 2013 ftunivnantes 2022-08-09T22:54:00Z Geochemical modeling is an interesting tool to assess the geochemical behavior of CO2 in the saline aquifer, including its dissolution in the brine and its interactions with minerals. The Pitzer interaction model is rarely used for simulating CO2 geochemical behavior in saline aquifers despite the fact that more conventionally used activity models are not valid for such salinities. A comparison between calculated mineral solubility evolution with salinity versus experimental data is performed here using both B-dot and Pitzer activity models as well as six different databases. This comparison exercise shows that chemical interactions within saline solutions can only be reproduced using the Pitzer model, even though Pitzer databases are still incomplete or are not coherent for a wide range of chemical species and temperatures. The geochemical simulations of CO2 injection in Ketzin, In Salah and Snøhvit saline aquifers give divergent results using different activity models and databases. A high uncertainty on the simulation results is then linked to the database choice and this study clearly stresses the need for a Pitzer database that can be confidently used in all physical/chemical conditions found in deep sedimentary aquifers. Conference Object Snøhvit Université de Nantes: HAL-UNIV-NANTES Norway
institution Open Polar
collection Université de Nantes: HAL-UNIV-NANTES
op_collection_id ftunivnantes
language English
topic CO2 storage
geochemical modeling
high salinity
Pitzer
dawsonite
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
spellingShingle CO2 storage
geochemical modeling
high salinity
Pitzer
dawsonite
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Tremosa, Joachim
Geochemical modeling of CO2 storage in saline aquifers: examples from Ketzin, In Salah and Snohvit storage sites
topic_facet CO2 storage
geochemical modeling
high salinity
Pitzer
dawsonite
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
description Geochemical modeling is an interesting tool to assess the geochemical behavior of CO2 in the saline aquifer, including its dissolution in the brine and its interactions with minerals. The Pitzer interaction model is rarely used for simulating CO2 geochemical behavior in saline aquifers despite the fact that more conventionally used activity models are not valid for such salinities. A comparison between calculated mineral solubility evolution with salinity versus experimental data is performed here using both B-dot and Pitzer activity models as well as six different databases. This comparison exercise shows that chemical interactions within saline solutions can only be reproduced using the Pitzer model, even though Pitzer databases are still incomplete or are not coherent for a wide range of chemical species and temperatures. The geochemical simulations of CO2 injection in Ketzin, In Salah and Snøhvit saline aquifers give divergent results using different activity models and databases. A high uncertainty on the simulation results is then linked to the database choice and this study clearly stresses the need for a Pitzer database that can be confidently used in all physical/chemical conditions found in deep sedimentary aquifers.
author2 Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)
format Conference Object
author Tremosa, Joachim
author_facet Tremosa, Joachim
author_sort Tremosa, Joachim
title Geochemical modeling of CO2 storage in saline aquifers: examples from Ketzin, In Salah and Snohvit storage sites
title_short Geochemical modeling of CO2 storage in saline aquifers: examples from Ketzin, In Salah and Snohvit storage sites
title_full Geochemical modeling of CO2 storage in saline aquifers: examples from Ketzin, In Salah and Snohvit storage sites
title_fullStr Geochemical modeling of CO2 storage in saline aquifers: examples from Ketzin, In Salah and Snohvit storage sites
title_full_unstemmed Geochemical modeling of CO2 storage in saline aquifers: examples from Ketzin, In Salah and Snohvit storage sites
title_sort geochemical modeling of co2 storage in saline aquifers: examples from ketzin, in salah and snohvit storage sites
publisher HAL CCSD
publishDate 2013
url https://hal-brgm.archives-ouvertes.fr/hal-00829892
op_coverage Trondheim, Norway
geographic Norway
geographic_facet Norway
genre Snøhvit
genre_facet Snøhvit
op_source IEAGHG Combined Modelling and Risk Management Network Meeting
https://hal-brgm.archives-ouvertes.fr/hal-00829892
IEAGHG Combined Modelling and Risk Management Network Meeting, Jun 2013, Trondheim, Norway
op_relation hal-00829892
https://hal-brgm.archives-ouvertes.fr/hal-00829892
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