Numerical Study of Gas Breakthrough in Preferential Rocks for Underground Nuclear Waste Repositories

During the long-term storage of radioactive waste, the continuous generation of gas in the disposal area may influence the integrity of host rock. Thus, the investigation of gas migration and breakthrough in low-permeability rock is indispensable for the stability assessment. In this work, the pore...

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Bibliographic Details
Published in:Minerals (Basel) 2023-03, Vol.13 (3), p.393
Main Authors: Zhang, Xiang, Yin, Hang, Yu, Wenjie, Lei, Zhen, Qu, Juntong
Format: Article
Language:English
Subjects:
Capillary pressure
Clay
Experiments
Fields (mathematics)
Fractures
gas breakthrough
Granite
Laboratories
Laplace equation
low-permeability rock
Mathematical models
Mathematical morphology
Methods
Morphology
Nuclear energy
Permeability
pore space model
Radioactive pollution
Radioactive waste sites
Radioactive wastes
random field
Rock
Rocks
Simulation
Stability analysis
Stone
Tomography
Underground storage
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Summary:During the long-term storage of radioactive waste, the continuous generation of gas in the disposal area may influence the integrity of host rock. Thus, the investigation of gas migration and breakthrough in low-permeability rock is indispensable for the stability assessment. In this work, the pore space models of four potential host rocks (Boom clay, COx argillite, Opalinus clay, and Beishan granite) were generated via the binarization of the Gaussian random field. This method provides a randomly formed pore network that does rely on an initial definition of pore shape. The constructed models were analyzed and validated by using the mathematical morphology. A numerical calculation scenario of gas breakthrough on the basis of the Young–Laplace equation was proposed and applied. Results show that the gas breakthrough pressures are 2.62–4.11 MPa in Boom clay and 3.72–4.27 MPa in COx argillite. It enhances the idea that the capillary-induced gas breakthrough is possible at pressures lower than the fracture threshold. For Opalinus clay and Beishan granite, no connected pathway exists, and the breakthrough is more likely to occur through pathway dilation or fractures. The presented method has the advantage of experimental reproducibility and brings a new idea for the investigation of fluid migration in low-permeability rocks.
ISSN:2075-163X
2075-163X
DOI:10.3390/min13030393