Temporal evolution of shear-induced dilatancy of rock fractures: controls from surface roughness and normal stress Article Swipe
YOU?
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· 2024
· Open Access
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· DOI: https://doi.org/10.1093/gji/ggae156
SUMMARY Understanding the shear-induced dilatancy of rock fractures is important for assessing the permeability evolution and seismic hazard in shale and geothermal reservoirs. The displacement dependence of fracture dilation has been well studied, while the influence of slip velocity is poorly constrained. In this study, we combined displacement- and velocity-dependent aperture models to reproduce the transient shear-induced dilatancy of fractures in sandstone in 16 normal stress unloading tests. Our results show that the combined aperture model can describe the transient fracture aperture evolution during accelerating slip induced by normal stress unloading better than the model dependent only on slip displacement. Slip velocity could enhance the aperture increase on smoother fractures at lower normal stresses and higher slip velocities. Both the dilation factor and characteristic slip distance decrease with increasing normal stress and surface roughness, signifying reduced contribution of slip velocity to transient shear-induced dilatancy at higher normal stresses and surface roughness. The dilation angle increases with the increase of surface roughness, and this increase diminishes at higher normal stresses primarily attributable to more severe asperity wear. These findings highlight the importance of slip velocity in controlling the transient evolution of aperture and permeability of a rock fracture. Our study also provides constraints on the constitutive parameters in the combined aperture model for describing transient shear-induced fracture dilatancy. We suggest that it is crucial to incorporate the velocity-dependent aperture model to simulate the nonlinear evolution of fracture aperture in future analytical and numerical models involving coupled hydromechanical processes in geoenergy systems.
Related Topics
- Type
- article
- Language
- en
- Landing Page
- https://doi.org/10.1093/gji/ggae156
- https://academic.oup.com/gji/advance-article-pdf/doi/10.1093/gji/ggae156/57356839/ggae156.pdf
- OA Status
- gold
- Cited By
- 1
- References
- 94
- Related Works
- 10
- OpenAlex ID
- https://openalex.org/W4396498612
Raw OpenAlex JSON
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https://openalex.org/W4396498612Canonical identifier for this work in OpenAlex
- DOI
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https://doi.org/10.1093/gji/ggae156Digital Object Identifier
- Title
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Temporal evolution of shear-induced dilatancy of rock fractures: controls from surface roughness and normal stressWork title
- Type
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articleOpenAlex work type
- Language
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enPrimary language
- Publication year
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2024Year of publication
- Publication date
-
2024-04-29Full publication date if available
- Authors
-
Supeng Zhang, Yinlin Ji, Hannes Hofmann, Qian Yin, Shouding Li, Yuanchao ZhangList of authors in order
- Landing page
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https://doi.org/10.1093/gji/ggae156Publisher landing page
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https://academic.oup.com/gji/advance-article-pdf/doi/10.1093/gji/ggae156/57356839/ggae156.pdfDirect link to full text PDF
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YesWhether a free full text is available
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goldOpen access status per OpenAlex
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https://academic.oup.com/gji/advance-article-pdf/doi/10.1093/gji/ggae156/57356839/ggae156.pdfDirect OA link when available
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Dilatant, Geology, Shear stress, Shear (geology), Surface roughness, Surface finish, Geotechnical engineering, Petrology, Composite material, Materials scienceTop concepts (fields/topics) attached by OpenAlex
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1Total citation count in OpenAlex
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2025: 1Per-year citation counts (last 5 years)
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10Other works algorithmically related by OpenAlex
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