2020
DOI: 10.1016/j.ijrmms.2019.104204
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Strength and deformability of a low-porosity sandstone under true triaxial compression conditions

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Cited by 41 publications
(11 citation statements)
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“…When confining pressure further increases, pure shear bands are predicted, in good accordance with experimental observations. 15 Finally, the sandstone is far from ductile regime under the experimental conditions. Compared with other porous sandstones, Zigong sandstone features a wide brittle range due to its low porosity.…”
Section: Effect Of Confining Pressure On Strain Localization Modementioning
confidence: 89%
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“…When confining pressure further increases, pure shear bands are predicted, in good accordance with experimental observations. 15 Finally, the sandstone is far from ductile regime under the experimental conditions. Compared with other porous sandstones, Zigong sandstone features a wide brittle range due to its low porosity.…”
Section: Effect Of Confining Pressure On Strain Localization Modementioning
confidence: 89%
“…Zigong sandstone represents a low-porosity (6.5%) hard sandstone composed mainly of silicate minerals, which has been systematically tested and investigated under different stress conditions. 8,14,15 Compared with other highly porous sandstones, Zigong sandstone features relatively higher strength and a wider brittle range. 15 It exhibits prominent characteristics of brittle fracturing even under a confining pressure (σ3) of as high as 80 MPa, approximately corresponding to a buried depth of 4 km.…”
Section: Experimental Materials and Experimental Proceduresmentioning
confidence: 99%
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“…The dependence of the compressibility coefficient of the pore volume on the value of the effective pressure has a pronounced non-linear character [25,26]. Therefore, it is important to know in what range of effective pressure changes the pore compressibility coefficient was estimated [27,28]. This prompted the authors to consider the available approaches to assessing compressibility in more details and choose from them the most accurate and adequately reflecting changes in the stress state of rocks that do not exceed their elastic and/or strength limit.…”
mentioning
confidence: 99%