Permeability Evolution and Frictional Stability of Fabricated Fractures With Specified Roughness
Abstract
Roughness is widely observed on natural fractures, and its impact on the potential for induced seismicity and associated fluid migration in the subsurface remains unclear. Here we perform fracture shearing and fluid flow experiments on artificially fabricated fractures with specified roughness to investigate the role of fracture roughness on frictional properties and permeability evolution. Given the experimental conditions, we observe that rough fractures show high roughness ratio S q/L w and return higher frictional strength due to the presence of cohesive interlocking asperities. Rough fracture surfaces show velocity strengthening behavior in the initial shearing stage, which may evolve to velocity neutral and velocity weakening at greater displacements—suggesting a dynamic weakening that rough fractures become less stable with shearing. The surface roughness exerts a dominant control on permeability evolution over the entire shearing history. Permeability declines monotonically by about 2 orders of magnitude for smooth fractures. For high roughness fractures, the permeabilities evolve episodically due to cycled compaction and dilation during shearing. With a slip distance of 6 to 8 mm, permeability of the rough surface may enhance up to an order of magnitude, but significant permeability reduction may also occur for rough samples when asperities are highly worn with gougemore »
- Authors:
-
- Univ. of Texas, Austin, TX (United States). Inst. for Geophysics; Pennsylvania State Univ., University Park, PA (United States). EMS Energy Inst., and G3 Center
- Pennsylvania State Univ., University Park, PA (United States). EMS Energy Inst., and G3 Center
- Pennsylvania State Univ., University Park, PA (United States). EMS Energy Inst., and G3 Center; National Inst. of Advanced Industrial Science and Technology, Koriyama (Japan). Fukushima Renewable Energy Inst.
- Tongji Univ., Shanghai (China)
- Publication Date:
- Research Org.:
- Pennsylvania State Univ., University Park, PA (United States)
- Sponsoring Org.:
- USDOE Office of Fossil Energy (FE)
- OSTI Identifier:
- 1614208
- Alternate Identifier(s):
- OSTI ID: 1480903
- Grant/Contract Number:
- FE0023354
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Journal of Geophysical Research. Solid Earth
- Additional Journal Information:
- Journal Volume: 123; Journal Issue: 11; Journal ID: ISSN 2169-9313
- Publisher:
- American Geophysical Union
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 58 GEOSCIENCES; Geochemistry & Geophysics; friction; permeability; fabricated fractures; specified roughness
Citation Formats
Fang, Yi, Elsworth, Derek, Ishibashi, Takuya, and Zhang, Fengshou. Permeability Evolution and Frictional Stability of Fabricated Fractures With Specified Roughness. United States: N. p., 2018.
Web. doi:10.1029/2018jb016215.
Fang, Yi, Elsworth, Derek, Ishibashi, Takuya, & Zhang, Fengshou. Permeability Evolution and Frictional Stability of Fabricated Fractures With Specified Roughness. United States. https://doi.org/10.1029/2018jb016215
Fang, Yi, Elsworth, Derek, Ishibashi, Takuya, and Zhang, Fengshou. Thu .
"Permeability Evolution and Frictional Stability of Fabricated Fractures With Specified Roughness". United States. https://doi.org/10.1029/2018jb016215. https://www.osti.gov/servlets/purl/1614208.
@article{osti_1614208,
title = {Permeability Evolution and Frictional Stability of Fabricated Fractures With Specified Roughness},
author = {Fang, Yi and Elsworth, Derek and Ishibashi, Takuya and Zhang, Fengshou},
abstractNote = {Roughness is widely observed on natural fractures, and its impact on the potential for induced seismicity and associated fluid migration in the subsurface remains unclear. Here we perform fracture shearing and fluid flow experiments on artificially fabricated fractures with specified roughness to investigate the role of fracture roughness on frictional properties and permeability evolution. Given the experimental conditions, we observe that rough fractures show high roughness ratio S q/L w and return higher frictional strength due to the presence of cohesive interlocking asperities. Rough fracture surfaces show velocity strengthening behavior in the initial shearing stage, which may evolve to velocity neutral and velocity weakening at greater displacements—suggesting a dynamic weakening that rough fractures become less stable with shearing. The surface roughness exerts a dominant control on permeability evolution over the entire shearing history. Permeability declines monotonically by about 2 orders of magnitude for smooth fractures. For high roughness fractures, the permeabilities evolve episodically due to cycled compaction and dilation during shearing. With a slip distance of 6 to 8 mm, permeability of the rough surface may enhance up to an order of magnitude, but significant permeability reduction may also occur for rough samples when asperities are highly worn with gouge clogging flow paths. However, there is no obvious correlation between permeability evolution and frictional behavior for rough fracture samples when fractures are subject to sudden sliding velocity changes.},
doi = {10.1029/2018jb016215},
journal = {Journal of Geophysical Research. Solid Earth},
number = 11,
volume = 123,
place = {United States},
year = {Thu Oct 04 00:00:00 EDT 2018},
month = {Thu Oct 04 00:00:00 EDT 2018}
}
Web of Science
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