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A coupled compressible flow and geomechanics model for dynamic fracture aperture during carbon sequestration in coal

Chen, Min; Hosking, Lee J.; Sandford, Richard J.; Thomas, Hywel R.

A coupled compressible flow and geomechanics model for dynamic fracture aperture during carbon sequestration in coal Thumbnail


Authors

Min Chen

Lee J. Hosking

Richard J. Sandford

Hywel R. Thomas



Abstract

This paper presents the development of a discrete fracture model of fully coupled compressible fluid flow, adsorption and geomechanics to investigate the dynamic behaviour of fractures in coal. The model is applied in the study of geological carbon dioxide sequestration and differs from the dual porosity model developed in our previous work, with fractures now represented explicitly using lower‐dimensional interface elements. The model consists of the fracture‐matrix fluid transport model, the matrix deformation model and the stress‐strain model for fracture deformation. A sequential implicit numerical method based on Galerkin finite element is employed to numerically solve the coupled governing equations, and verification is completed using published solutions as benchmarks. To explore the dynamic behaviour of fractures for understanding the process of carbon sequestration in coal, the model is used to investigate the effects of gas injection pressure and composition, adsorption and matrix permeability on the dynamic behaviour of fractures. The numerical results indicate that injecting nonadsorbing gas causes a monotonic increase in fracture aperture; however, the evolution of fracture aperture due to gas adsorption is complex due to the swelling‐induced transition from local swelling to macro swelling. The change of fracture aperture is mainly controlled by the normal stress acting on the fracture surface. The fracture aperture initially increases for smaller matrix permeability and then declines after reaching a maximum value. When the local swelling becomes global, fracture aperture starts to rebound. However, when the matrix permeability is larger, the fracture aperture decreases before recovering to a higher value and remaining constant. Gas mixtures containing more carbon dioxide lead to larger closure of fracture aperture compared with those containing more nitrogen.

Citation

Chen, M., Hosking, L. J., Sandford, R. J., & Thomas, H. R. (2020). A coupled compressible flow and geomechanics model for dynamic fracture aperture during carbon sequestration in coal. International Journal for Numerical and Analytical Methods in Geomechanics, 44(13), 1727-1749. https://doi.org/10.1002/nag.3075

Journal Article Type Article
Acceptance Date Mar 27, 2020
Online Publication Date May 26, 2020
Publication Date Sep 1, 2020
Deposit Date Sep 8, 2020
Publicly Available Date Sep 8, 2020
Journal International Journal for Numerical and Analytical Methods in Geomechanics
Print ISSN 0363-9061
Electronic ISSN 1096-9853
Publisher Wiley
Peer Reviewed Peer Reviewed
Volume 44
Issue 13
Pages 1727-1749
DOI https://doi.org/10.1002/nag.3075
Keywords Geotechnical engineering and engineering geology; General materials science; Mechanics of materials; Computational mechanics; Adsorption; Carbon sequestration; Coal swelling; Discrete fracture model; Fracture deformation
Public URL https://uwe-repository.worktribe.com/output/6004284
Additional Information Received: 2019-09-25; Accepted: 2020-03-27; Published: 2020-05-26

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Licence
http://creativecommons.org/licenses/by/4.0/

Publisher Licence URL
http://creativecommons.org/licenses/by/4.0/

Copyright Statement
© 2020 The Authors. International Journal for Numerical and Analytical Methods in Geomechanics published by John Wiley & Sons Ltd

This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.




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