X-ray micro-computed tomography and ultrasonic velocity analysis of fractured shale as a function of effective stress

© 2019 Elsevier Ltd Ultrasonic velocity is a key shale gas reservoir property, especially in the context of gas production or CO2 injection for geo-sequestration. This ultrasonic velocity reflects the dynamic elastic properties of the rock, and it thus depends on the fracture morphology, which v...

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Main Authors: Yu, H., Zhang, Y., Lebedev, Maxim, Wang, Z., Li, X., Squelch, Andrew, Verrall, M., Iglauer, Stefan
Format: Journal Article
Language:English
Published: ELSEVIER SCI LTD 2019
Subjects:
Online Access:http://hdl.handle.net/20.500.11937/79269
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author Yu, H.
Zhang, Y.
Lebedev, Maxim
Wang, Z.
Li, X.
Squelch, Andrew
Verrall, M.
Iglauer, Stefan
author_facet Yu, H.
Zhang, Y.
Lebedev, Maxim
Wang, Z.
Li, X.
Squelch, Andrew
Verrall, M.
Iglauer, Stefan
author_sort Yu, H.
building Curtin Institutional Repository
collection Online Access
description © 2019 Elsevier Ltd Ultrasonic velocity is a key shale gas reservoir property, especially in the context of gas production or CO2 injection for geo-sequestration. This ultrasonic velocity reflects the dynamic elastic properties of the rock, and it thus depends on the fracture morphology, which varies significantly with effective stress. However, the precise relationship between ultrasonic velocity and fractured shale morphology is only poorly understood. We thus measured P- and S-wave velocities of fractured shale in two orthogonal directions and imaged the shale with X-ray micro-computed tomography as a function of applied effective stress; and investigated how fracture morphology, P- and S-wave velocity, Young's modulus, shear velocity and Poisson's ratio are interconnected with effective stress. Clearly, most of the small fractures (the width is around 0.1 mm) closed with increasing effective stress, resulting in a different fracture size distribution, which again had a dramatic effect on the elastic rock properties. Furthermore, with increasing effective stress, P- and S-wave velocities increased significantly, such that the orthogonal waves gave a similar response at 2000 psi effective stress despite significant sample heterogeneity. We conclude that the fracture aperture, direction and network characteristics severely influence wave propagation and thus elastic properties. These results can be used to assess natural fracture networks, monitor fracture development during hydraulic fracturing, and predict fracture closure scenarios during production.
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spelling curtin-20.500.11937-792692020-08-04T03:02:58Z X-ray micro-computed tomography and ultrasonic velocity analysis of fractured shale as a function of effective stress Yu, H. Zhang, Y. Lebedev, Maxim Wang, Z. Li, X. Squelch, Andrew Verrall, M. Iglauer, Stefan Science & Technology Physical Sciences Geosciences, Multidisciplinary Geology Ultrasonic Fractured shale microCT Elastic properties ELASTIC PROPERTIES WAVE-PROPAGATION PARALLEL FRACTURES PERMEABILITY COAL ATTENUATION ROCKS CT EVOLUTION PRESSURE © 2019 Elsevier Ltd Ultrasonic velocity is a key shale gas reservoir property, especially in the context of gas production or CO2 injection for geo-sequestration. This ultrasonic velocity reflects the dynamic elastic properties of the rock, and it thus depends on the fracture morphology, which varies significantly with effective stress. However, the precise relationship between ultrasonic velocity and fractured shale morphology is only poorly understood. We thus measured P- and S-wave velocities of fractured shale in two orthogonal directions and imaged the shale with X-ray micro-computed tomography as a function of applied effective stress; and investigated how fracture morphology, P- and S-wave velocity, Young's modulus, shear velocity and Poisson's ratio are interconnected with effective stress. Clearly, most of the small fractures (the width is around 0.1 mm) closed with increasing effective stress, resulting in a different fracture size distribution, which again had a dramatic effect on the elastic rock properties. Furthermore, with increasing effective stress, P- and S-wave velocities increased significantly, such that the orthogonal waves gave a similar response at 2000 psi effective stress despite significant sample heterogeneity. We conclude that the fracture aperture, direction and network characteristics severely influence wave propagation and thus elastic properties. These results can be used to assess natural fracture networks, monitor fracture development during hydraulic fracturing, and predict fracture closure scenarios during production. 2019 Journal Article http://hdl.handle.net/20.500.11937/79269 10.1016/j.marpetgeo.2019.07.015 English ELSEVIER SCI LTD restricted
spellingShingle Science & Technology
Physical Sciences
Geosciences, Multidisciplinary
Geology
Ultrasonic
Fractured shale
microCT
Elastic properties
ELASTIC PROPERTIES
WAVE-PROPAGATION
PARALLEL FRACTURES
PERMEABILITY
COAL
ATTENUATION
ROCKS
CT
EVOLUTION
PRESSURE
Yu, H.
Zhang, Y.
Lebedev, Maxim
Wang, Z.
Li, X.
Squelch, Andrew
Verrall, M.
Iglauer, Stefan
X-ray micro-computed tomography and ultrasonic velocity analysis of fractured shale as a function of effective stress
title X-ray micro-computed tomography and ultrasonic velocity analysis of fractured shale as a function of effective stress
title_full X-ray micro-computed tomography and ultrasonic velocity analysis of fractured shale as a function of effective stress
title_fullStr X-ray micro-computed tomography and ultrasonic velocity analysis of fractured shale as a function of effective stress
title_full_unstemmed X-ray micro-computed tomography and ultrasonic velocity analysis of fractured shale as a function of effective stress
title_short X-ray micro-computed tomography and ultrasonic velocity analysis of fractured shale as a function of effective stress
title_sort x-ray micro-computed tomography and ultrasonic velocity analysis of fractured shale as a function of effective stress
topic Science & Technology
Physical Sciences
Geosciences, Multidisciplinary
Geology
Ultrasonic
Fractured shale
microCT
Elastic properties
ELASTIC PROPERTIES
WAVE-PROPAGATION
PARALLEL FRACTURES
PERMEABILITY
COAL
ATTENUATION
ROCKS
CT
EVOLUTION
PRESSURE
url http://hdl.handle.net/20.500.11937/79269