Density-Driven Convection in a Fractured Porous Media: Implications for Geological CO2 Storage

Minji Kim, Kue Young Kim, Weon Shik Han, Junho Oh, Eungyu Park

Research output: Contribution to journalArticlepeer-review

3 Citations (Scopus)

Abstract

Dissolution trapping is one of the primary mechanisms of carbon dioxide (CO2) storage in a geological formation. In this study, a numerical model was used to examine the impacts of single and multiple fractures on the transport of dissolved CO2 plumes in various geological settings. The effects of the fracture angle, fracture-matrix permeability ratio, fracture intersection, and matrix heterogeneity on density-driven CO2 convection were systematically investigated. The fractures were found to play time-varying roles in both homogeneous and heterogeneous media by serving as preferential pathways for both CO2-rich plumes (fingers) and CO2-free water. The competition between the enhancement of convective mixing and the inhibition of finger growth by the upward flow of freshwater generated a complex flow system. The interaction between the strong upward flow of freshwater through the fractures and the falling CO2-rich fingers through the porous matrix induced a positive feedback, resulting in accelerated domain-scale circulation and CO2 dissolution. While the CO2-rich fingers grew relatively evenly at the top boundary in the homogeneous media, they selectively developed through the high permeable zones in the heterogeneous media. Compared with homogeneous media, the heterogeneous media preserving fractures particularly generated a more dynamic fracture-matrix mass transfer, resulting in more rapid CO2 dissolution. The findings of this study were extended to examine the effects of fracture connectivity on the enhancement of CO2 transport and dissolution on a field scale.

Original languageEnglish
Pages (from-to)5852-5870
Number of pages19
JournalWater Resources Research
Volume55
Issue number7
DOIs
Publication statusPublished - 2019

Bibliographical note

Funding Information:
This research was supported by the Basic Research Project of the Korea Institute of Geoscience and Mineral Resources (KIGAM) funded by the Ministry of Science and ICT. Additional support was provided by Korea Environment Industry & Technology Institute (KEITI) through the Subsurface Environment Management (SEM) Project, funded by the Korea Ministry of Environment (MOE; 2018002440004 and 2018002440003). The authors thank the Editor and three anonymous reviewers for their valuable comments that greatly contributed to improving the article. The simulation data of this study are available from the public data sharing site Zenodo at the following address: https://doi.org/10.5281/Zenodo.3250418.

Publisher Copyright:
©2019. American Geophysical Union. All Rights Reserved.

All Science Journal Classification (ASJC) codes

  • Water Science and Technology

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