The responses of electrical resistivity tool to CO2 dissolution in brine and carbon mineralization – Implication for Monitoring Underground CO2 Sequestration.

Evaluation of the reliability of CO2 monitoring techniques is a critical step in risk assessment ofany CCS project. Electrical resistivity survey has an edge over seismic survey as a tool to monitor CO2plume migration, mainly due to the insensitivity of the latter to CO2 saturation above 20%. However, theability of electrical resistivity sensors to track CO2 dissolution in aquifer brine and then carbonmineralization that occurs afterwards is still not very convincing as shown by the conflicting experimentaland field data published in the literature. The objectives of this paper include a review of publishedexperimental and field data, present more experimental data to clear some doubts and then use theknowledge gained therein to produce an electrical resistivity response model to the different geochemicalprocesses that take place in the life cycle of CO2 storage in underground aquifer formation. Here, threedifferent types of laboratory experiments are presented to enhance our understanding of the responses ofelectrical resistivity to: (1) CO2 plume migration in a saline aquifer, (2) CO2 dissolution in aquifer brine, (3)CO2 mineralization process in a carbonate rock. Laboratory flow and static experimental systems were setup, which consist of flow pumps, an industrial oven, pressure and temperature transducers, core (sample)holder, an electrical resistivity meter that is able to log electrical resistivity measurements at high pressureand high temperature, and a data logging computer for monitoring and storing the measured data. The threeexperiments showed that electrical resistivity: (1) is highly sensitive to CO2 plume migration (2) isinsensitive to CO2 dissolution in aquifer brine, (3) is sensitive to rock dissolution and the subsequentmineralization process. An explanation is provided why electrical resistivity is insensitive to CO2 dissolutionin aquifer brine. Also, a validation experiment was conducted to validate the response of electrical resistivityto carbon mineralization. Finally, an electrical resistivity response model was developed to describe thebehaviour of resistivity to the different geochemical processes during CO2 underground storage process.

Institutions

Publication Details

Journal
Zenodo (CERN European Organization for Nuclear Research)
Published
2025-08-25
DOI
https://doi.org/10.5281/zenodo.16814281
Primary Topic
CO2 Sequestration and Geologic Interactions
Type
article
Field-Weighted Citation Impact
0.00
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

The responses of electrical resistivity tool to CO2 dissolution in brine and carbon mineralization – Implication for Monitoring Underground CO2 Sequestration.

Zenodo (CERN European Organization for Nuclear Research)
CO2 Sequestration and Geologic Interactions
article

The responses of electrical resistivity tool to CO2 dissolution in brine and carbon mineralization – Implication for Monitoring Underground CO2 Sequestration.

article en

Abstract

Evaluation of the reliability of CO2 monitoring techniques is a critical step in risk assessment ofany CCS project. Electrical resistivity survey has an edge over seismic survey as a tool to monitor CO2plume migration, mainly due to the insensitivity of the latter to CO2 saturation above 20%. However, theability of electrical resistivity sensors to track CO2 dissolution in aquifer brine and then carbonmineralization that occurs afterwards is still not very convincing as shown by the conflicting experimentaland field data published in the literature. The objectives of this paper include a review of publishedexperimental and field data, present more experimental data to clear some doubts and then use theknowledge gained therein to produce an electrical resistivity response model to the different geochemicalprocesses that take place in the life cycle of CO2 storage in underground aquifer formation. Here, threedifferent types of laboratory experiments are presented to enhance our understanding of the responses ofelectrical resistivity to: (1) CO2 plume migration in a saline aquifer, (2) CO2 dissolution in aquifer brine, (3)CO2 mineralization process in a carbonate rock. Laboratory flow and static experimental systems were setup, which consist of flow pumps, an industrial oven, pressure and temperature transducers, core (sample)holder, an electrical resistivity meter that is able to log electrical resistivity measurements at high pressureand high temperature, and a data logging computer for monitoring and storing the measured data. The threeexperiments showed that electrical resistivity: (1) is highly sensitive to CO2 plume migration (2) isinsensitive to CO2 dissolution in aquifer brine, (3) is sensitive to rock dissolution and the subsequentmineralization process. An explanation is provided why electrical resistivity is insensitive to CO2 dissolutionin aquifer brine. Also, a validation experiment was conducted to validate the response of electrical resistivityto carbon mineralization. Finally, an electrical resistivity response model was developed to describe thebehaviour of resistivity to the different geochemical processes during CO2 underground storage process.

Zenodo (CERN European Organization for Nuclear Research)
King Fahd University of Petroleum and Minerals (SA)
Responsible consumption and production
Openalex Percentile: Top 59%
CO2 Sequestration and Geologic Interactions
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.