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A feasibility study of CO2 sequestration monitoring using the mCSEM method at a deep brine aquifer in a shallow sea

Authors
Kang, SeogiSeol, Soon JeeByun, Joongmoo
Issue Date
Mar-2012
Publisher
SOC EXPLORATION GEOPHYSICISTS
Keywords
Electromagnetics; Finite element; Modeling; Monitoring
Citation
GEOPHYSICS, v.77, no.2, pp.E117 - E126
Indexed
SCIE
SCOPUS
Journal Title
GEOPHYSICS
Volume
77
Number
2
Start Page
E117
End Page
E126
URI
https://scholarworks.bwise.kr/hanyang/handle/2021.sw.hanyang/166141
DOI
10.1190/GEO2011-0089.1
ISSN
0016-8033
Abstract
Reservoir production monitoring using marine controlled-source electromagnetic (mCSEM) has been studied recently because it is sensitive to resistivity changes resulting from variations in hydrocarbon saturation. However, mCSEM for CO2 sequestration monitoring has scarcely been investigated, although the mCSEM method is advantageous for monitoring CO2 injection and migration. To investigate the feasibility of inCSEM monitoring for CO2 sequestration, we conducted numerical experiments of representative CO2 injection models at a deep brine aquifer in a shallow sea. By using a modified secondary field method, we effectively address the airwave problem occurring when mCSEM is applied to a target beneath a shallow sea. We demonstrate the modified secondary field method can restore high frequency band data, which is beneficial for the detection of the movement of injected CO2. Furthermore, using a modified scattered field approach for 2.5D forward modeling, we achieve very high accuracy, which is essential for the simulation of electromagnetic fields generated by CO2 injection in a deep brine aquifer. The mCSEM response, which is enhanced by the modified secondary field method, shows small but measurable changes in a given pseudorealistic CO2 sequestration scenario. The inCSEM responses differ for horizontal and vertical injections. These results include the feasibility of applying mCSEM to CO2 sequestration monitoring. Optimum operating frequency bands and source-receiver geometries for a brine aquifer model beneath a shallow sea are proposed based on the results of the numerical experiments. Moreover, we suggest the necessity or various types of data acquisition for the monitoring of a CO2 plume based on analyses of multiple components of electric and magnetic fields.
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