Abstract
Spatial distribution of sand bodies in caprock is important to its sealing potential in the evaluation of a potential waste disposal site. A numerical investigation was conducted to investigate the roles of sand bodies in caprock integrity, and a new leaking mechanism associated with the embedded sand bodies has been identified for the first time. This numerical model is characterized by a low proportion of sand bodies in caprock formation and stochastic permeability assignments to the shale facies with a consideration of stress-sensitive permeability. The research revealed that sand bodies in caprock, even initially unconnected due to their low concentration, represent the foundation for creating a percolating flow path if certain conditions are met. These conditions include a relatively high pore pressure gradient across the caprock, which may occur during fluid injection and a favorable geometric configuration of these sand bodies. Sand bodies of different shapes play different roles in forming a percolating flow path. Sand bars/dykes can lead pore pressure front to cover a considerable vertical thickness quickly, while thin sand sheets tend to transfer the pore pressure front across a large horizontal range and thus increase the possibility of involving other local sand bodies in the evolution of percolating flow paths. On the other hand, the presence of percolating flow path in caprock can limit the pore pressure increase in the aquifer formation during fluid injection. The more active the flow paths, the less increase the pore pressure that occurs in the aquifer. Stress-dependent permeability can facilitate the formation of percolating flow path, but evaluating how much impact it may have remains a question for future research. The modeling results indicate that the underlying geologically based discrete structure of permeable domains, even when masked by a low-permeable rock matrix, exerts a significant influence on the location and magnitude of fluid flow within the system during fluid injection.
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Acknowledgments
This technical effort was performed in support of the National Energy Technology Laboratory’s ongoing research in geologic CO2 sequestration under the RES contract DE-FE0004000. Any opinions, findings, and conclusions expressed in this material are those of the authors and do not necessarily state or reflect the views of the US Government or any agency thereof. We appreciate anonymous reviewers for providing very helpful comments to improve the quality of this paper.
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Zhou, X., Burbey, T.J. Numerical modeling of percolating flow path in a caprock formation during aquifer pressurization and its implication for CO2 sequestration. Environ Earth Sci 75, 861 (2016). https://doi.org/10.1007/s12665-016-5679-1
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DOI: https://doi.org/10.1007/s12665-016-5679-1