High-stress triaxial direct-shear fracturing of Utica shale and in situ X-ray microtomography with permeability measurement
Abstract
The challenge of characterizing subsurface fluid flow has motivated extensive laboratory studies, yet fluid flow through rock specimens in which fractures are created and maintained at high-stress conditions remains underinvestigated at this time. The studies of this type that do exist do not include in situ fracture geometry measurements acquired at stressed conditions, which would be beneficial for interpreting the flow behavior. Therefore, this study investigates the apparent permeability induced by direct-shear fracture stimulation through Utica shale (a shale gas resource and potential caprock material) at high triaxial stress confinement and for the first time relates these values to simultaneously acquired in situ X-ray radiography and microtomography images. Change in fracture geometry and apparent permeability was also investigated at additional reduced stress states. Finite element and combined finite-discrete element modeling were used to evaluate the in situ observed fracturing process. Results from this study indicate that the increase in apparent permeability through fractures created at high-stress (22.2 MPa) was minimal relative to the intact rock (less than 1 order of magnitude increase), while fractures created at low stress (3.4 MPa) were significantly more permeable (2 to 4 orders of magnitude increase). Here, this study demonstrates the benefit of in situmore »
- Authors:
-
- Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
- Publication Date:
- Research Org.:
- Los Alamos National Laboratory (LANL), Los Alamos, NM (United States)
- Sponsoring Org.:
- USDOE
- OSTI Identifier:
- 1532704
- Alternate Identifier(s):
- OSTI ID: 1402279
- Report Number(s):
- LA-UR-15-27278
Journal ID: ISSN 2169-9313
- Grant/Contract Number:
- 89233218CNA000001
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Journal of Geophysical Research. Solid Earth
- Additional Journal Information:
- Journal Volume: 121; Journal Issue: 7; Journal ID: ISSN 2169-9313
- Publisher:
- American Geophysical Union
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 58 GEOSCIENCES; Energy Sciences; X-ray Computed Tomography; Utica; Shale; Fracture; Permeability; Microtomography; CO2 sequestration; Hydraulic Fracturing; Shear Stimulation; Caprock; FDEM; Induced Seismicity
Citation Formats
Frash, Luke P., Carey, J. William, Lei, Zhou, Rougier, Esteban, Ickes, Timothy, and Viswanathan, Hari S. High-stress triaxial direct-shear fracturing of Utica shale and in situ X-ray microtomography with permeability measurement. United States: N. p., 2016.
Web. doi:10.1002/2016JB012850.
Frash, Luke P., Carey, J. William, Lei, Zhou, Rougier, Esteban, Ickes, Timothy, & Viswanathan, Hari S. High-stress triaxial direct-shear fracturing of Utica shale and in situ X-ray microtomography with permeability measurement. United States. https://doi.org/10.1002/2016JB012850
Frash, Luke P., Carey, J. William, Lei, Zhou, Rougier, Esteban, Ickes, Timothy, and Viswanathan, Hari S. Sat .
"High-stress triaxial direct-shear fracturing of Utica shale and in situ X-ray microtomography with permeability measurement". United States. https://doi.org/10.1002/2016JB012850. https://www.osti.gov/servlets/purl/1532704.
@article{osti_1532704,
title = {High-stress triaxial direct-shear fracturing of Utica shale and in situ X-ray microtomography with permeability measurement},
author = {Frash, Luke P. and Carey, J. William and Lei, Zhou and Rougier, Esteban and Ickes, Timothy and Viswanathan, Hari S.},
abstractNote = {The challenge of characterizing subsurface fluid flow has motivated extensive laboratory studies, yet fluid flow through rock specimens in which fractures are created and maintained at high-stress conditions remains underinvestigated at this time. The studies of this type that do exist do not include in situ fracture geometry measurements acquired at stressed conditions, which would be beneficial for interpreting the flow behavior. Therefore, this study investigates the apparent permeability induced by direct-shear fracture stimulation through Utica shale (a shale gas resource and potential caprock material) at high triaxial stress confinement and for the first time relates these values to simultaneously acquired in situ X-ray radiography and microtomography images. Change in fracture geometry and apparent permeability was also investigated at additional reduced stress states. Finite element and combined finite-discrete element modeling were used to evaluate the in situ observed fracturing process. Results from this study indicate that the increase in apparent permeability through fractures created at high-stress (22.2 MPa) was minimal relative to the intact rock (less than 1 order of magnitude increase), while fractures created at low stress (3.4 MPa) were significantly more permeable (2 to 4 orders of magnitude increase). Here, this study demonstrates the benefit of in situ X-ray observation coupled with apparent permeability measurement to analyze fracture creation in the subsurface. Our results show that the permeability induced by fractures through shale at high stress can be minor and therefore favorable in application to CO2 sequestration caprock integrity but unfavorable for hydrocarbon recovery from unconventional reservoirs.},
doi = {10.1002/2016JB012850},
journal = {Journal of Geophysical Research. Solid Earth},
number = 7,
volume = 121,
place = {United States},
year = {Sat Jul 09 00:00:00 EDT 2016},
month = {Sat Jul 09 00:00:00 EDT 2016}
}
Web of Science
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