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      Failure characteristics of two porous sandstones subjected to true triaxial stresses: Applied through a novel loading path

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          Abstract

          We performed an extensive suite of true triaxial experiments in two porous sandstones, Bentheim (porosity ≈ 24%) and Coconino (17%). The experiments were conducted using a novel loading path, which maintains constant Lode angle ( Θ) throughout the test. This path enabled the examination of the effects of Lode angle and mean stress on failure ( σ oct,f). Our tests covered σ 3 magnitudes between 0 and 150 MPa and of Θ at −30° (axisymmetric extension), −16°, 0°, +11°, +21°, and +30° (axisymmetric compression). Test results revealed the respective contribution of each of the two stress invariants to failure stress, failure plane angle, and failure mode. In both sandstones, the shear stress required for failure increases with mean stress but decreases with Θ when shear failure mode dominates. However, the dependence of failure stress on mean stress and Θ is reversed when the compactive failure mode is in control. The compactive failure mode was evident in Bentheim sandstone when compaction bands were observed under high mean stress. The Coconino sandstone did not reach the compactive failure regime within the maximum confinement applied. The failure plane angle monotonically decreases with increasing mean stress and Θ. For Coconino sandstone, failure plane angle varies between 80° and 50° for σ oct,f between 50 and 450 MPa whereas it drops to 0° as σ oct,f, approaches 250 MPa in Bentheim sandstone. We employed the bifurcation theory to relate the stress conditions at failure to the development of failure planes. The theory is in qualitative agreement with the experimental data.

          Key Points

          • Lode angle affects failure stress, failure plane angle, and failure mode

          • Failure‐mode evolution from shear to compactive failure with mean stress in Bentheim sandstone is more prominent than in Coconino

          • Predictions of failure plane angle via bifurcation theory agree qualitatively with experimental data

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          Most cited references43

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          Limits on lithospheric stress imposed by laboratory experiments

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            Conditions for the localization of deformation in pressure-sensitive dilatant materials

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              State of Stress in the Earth's Crust

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                Author and article information

                Contributors
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                Journal
                Journal of Geophysical Research: Solid Earth
                JGR Solid Earth
                Wiley
                2169-9313
                2169-9356
                April 2017
                April 15 2017
                April 2017
                : 122
                : 4
                : 2525-2540
                Affiliations
                [1 ] Geological Engineering Program and Department of Materials Science and Engineering University of Wisconsin‐Madison Madison Wisconsin USA
                [2 ] Now at Department of Geophysics Stanford University Stanford California USA
                [3 ] Department of Civil and Environmental Engineering and Department of Mechanical Engineering Northwestern University Evanston Illinois USA
                Article
                10.1002/2016JB013637
                e81f9ffb-8fa2-4b7a-b794-e505da6c2728
                © 2017

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