4.5 Article Proceedings Paper

Multistep triaxial strength tests: Investigating strength parameters and pore pressure effects on Opalinus Clay

Journal

PHYSICS AND CHEMISTRY OF THE EARTH
Volume 36, Issue 17-18, Pages 1898-1904

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.pce.2011.07.024

Keywords

Strength test; Opalinus Clay; Poroelastic coupling; Shear strength; Residual strength; Anisotropy

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Natural variability between rock samples often hampers a detailed analysis of material properties. For the investigation of strength parameters the concept of multistep triaxial strength tests was developed to avoid the impact of sample variability. The limit of linear elastic behavior, shear strength and residual strength were measured at different confining pressure on a single specimen. Appropriate tools for near real time data analysis were developed to facilitate a precise and timely control of the test procedure. This is essential to minimize the problem of sample degradation during the test. The feasibility of the test concept was proven on three samples of Opalinus Clay from the Mont Terri rock laboratory. Each investigated strength parameter displayed a distinct deviation from a linear dependency on confining pressure or mean stress respectively. Instead, curves consisting of two linear branches almost perfectly fit the test results. These results could be explained in the framework of poroelastic theory. Although it is not possible to determine Skempton's B-parameter (Skempton, 1954) and the Biot-Willis poroelastic parameter (Blot and Willis, 1957) separately from multistep strength tests, the product of both parameters can be derived from the test results. Although material anisotropy was found by the test results, numerous simple strength tests (Grasle and Plischke, 2010) as well as true triaxial tests (Naumann et al., 2007) provide a more efficient way to investigate anisotropy. (C) 2011 Elsevier Ltd. All rights reserved.

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