Technical Papers
Nov 30, 2019

Comprehensive Evaluation of Strength Criteria for Granite, Marble, and Sandstone Based on Polyaxial Experimental Tests

Publication: International Journal of Geomechanics
Volume 20, Issue 2

Abstract

Cubic specimens of three rocks—granite, marble, and sandstone, representing very strong rock, moderately strong rock, and weak rock, respectively—were tested under polyaxial stress. The objective was to determine the optimal strength criteria for these rocks by using the polyaxial test data. Experimental results indicated that the failure strength considerably depended on σ2 and σ3 for all the rocks. Seven well-known rock-strength criteria were employed to examine the true-triaxial data with regard to the predictability in practical applications, comparison between the best-fitting functions (experimental data) and theoretical (predicted) solutions, stress trajectories on the deviatoric plane, and stress trajectories on the meridian plane and τoctσoct space. A detailed analysis and comparison of these criteria showed that the Mogi–Coulomb criterion, modified Wiebols–Cook criterion, and modified Lade criterion provided a better prediction of the polyaxial strength for the three rocks in most cases, which is attributed to the high σ2 dependence and sensitivity of the selected rocks. The Mogi 1971 and 1967 criteria could not be correlated to the strength parameters (cohesion and frictional angle) and failed to predict the real strength values of an in situ rock mass without complex polyaxial compression tests. Furthermore, the stress trajectories on the deviatoric plane illustrated their disadvantages in theoretical interpretation and numerical implementation. The inferiority of the Mohr–Coulomb criterion and Drucker–Prager (DP) criterion in describing the rock strength under polyaxial stress was verified by the higher deviation between the theoretical (predicted) strength values and experimental strength values. The nonconformity between the stress trajectories and experimental data for the Mohr–Coulomb criterion and DP criterion on the meridian plane and in the τoctσoct space validates the preceding viewpoint.

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Acknowledgments

The authors acknowledge the financial support of the State Key Research Development Program of China (2016 YFC0600706), the Key projects of National Natural Science Foundation (Grant No. 41630642), and the National Natural Science Foundation of China (Grants Nos. 51474250 and 51774326). Kun Du was supported by the Natural Science Foundation of Hunan Province, China (Grant No. 2017JJ3390), the China Postdoctoral Science Foundation (Grant No. 2016M602432), and the Key Laboratory of Deep Coal Mine Excavation Response and Disaster Prevention and Control at Anhui University of Science and Technology (Grant No. KLDCMERDPC15104).

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Go to International Journal of Geomechanics
International Journal of Geomechanics
Volume 20Issue 2February 2020

History

Received: Jun 20, 2018
Accepted: May 30, 2019
Published online: Nov 30, 2019
Published in print: Feb 1, 2020
Discussion open until: Apr 30, 2020

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Fan Feng
Lecturer, College of Mining and Safety Engineering, Shandong Univ. of Science and Technology, Qingdao, Shandong 266590, China; School of Resources and Safety Engineering, Central South Univ., Changsha, Hunan 410083, China.
Xibing Li
Professor, School of Resources and Safety Engineering, Central South Univ., Changsha, Hunan 410083, China.
Associate Professor, School of Resources and Safety Engineering, Central South Univ., Changsha, Hunan 410083, China (corresponding author). Email: [email protected]
Diyuan Li
Professor, School of Resources and Safety Engineering, Central South Univ., Changsha, Hunan 410083, China.
Jamal Rostami, M.ASCE
Associate Professor, Earth Mechanics Institute, Dept. of Mining Engineering, Colorado School of Mines, Golden, CO 80401.
Lecturer, School of Resources and Safety Engineering, Central South Univ., Changsha, Hunan 410083, China. ORCID: https://orcid.org/0000-0001-9870-6463

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