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New Peak Shear Strength Criterion of Rock Joints Based on Quantified Surface Description

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Abstract

The prime objective of this work is to improve our understanding of the shear behavior of rock joints. Attempts are made to relate the peak shear strength of rock joints with its three-dimensional surface morphology parameters. Three groups of tensile joint replicas with different surface morphology are tested with direct shear tests under constant normal load (CNL) conditions. Firstly, the three-dimensional surface characterization of these joints is evaluated by an improved roughness parameter before being tested. Then, a new empirical criterion is proposed for these joints expressed by three-dimensional quantified surface roughness parameters without any averaging variables in such a way that a rational dilatancy angle function is used instead of \({\text{JRC}} \cdot \log_{10} \left( {{{\text{JCS}} \mathord{\left/ {\vphantom {{\text{JCS}} {\sigma_{\text{n}} }}} \right. \kern-\nulldelimiterspace} {\sigma_{\text{n}} }}} \right)\) by satisfying the new peak dilatancy angle boundary conditions under zero and critical-state normal stress (not physical infinite normal stress). The proposed criterion has the capability of estimating the peak shear strength at the laboratory scale and the required roughness parameters can be easily measured. Finally, a comparison among the proposed criterion, Grasselli’s criterion, and Barton’s criterion are made from the perspective of both the rationality of the formula and the prediction accuracy for the three groups of joints. The limitations of Grasselli’s criterion are analyzed in detail. Another 37 experimental data points of fresh rock joints by Grasselli are used to further verify the proposed criterion. Although both the proposed criterion and Grasselli’s criterion have almost equal accuracy of predicting the peak shear strength of rock joints, the proposed criterion is easier and more intuitive from an engineering point of view because of its Mohr–Coulomb type of formulation.

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Abbreviations

A 0 :

Normalized area corresponding to the apparent dip angle \(\theta_{\max }^{*}\) = 0

\(A_{{\theta^{*} }}\) :

Normalized area corresponding to the apparent dip angle θ *

C :

Roughness parameter characterizing the distribution of apparent dip angles over the joint surface

d n :

Dilatancy angle (°)

d n,0 :

Dilatancy angle at zero normal stress (°)

d n,peak :

Peak dilatancy angle (°)

d n,crit :

Critical dilatancy angle at the critical normal stress (°)

JCS:

Joint wall compressive strength (MPa)

JRC:

Joint roughness coefficient

JRCcal :

Value of JRC obtained by the direct shear test

JRCtilt :

Value of JRC obtained by the tilt test

JRCvisual :

Value of JRC obtained by the visual method

JRC j :

JRC value of the jth profile along the shear direction

Ave:

Average value

SD:

Standard deviation

Max:

Maximum value

Min:

Minimum value

d :

True dip vector

t :

Shear vector

w :

Shear plane

α:

Azimuth (°)

β:

Angle between the schistosity plane and the plane normal to the joint (°)

θ :

Dip angle (°)

θ * :

Apparent dip angle of each triangle along the shear direction (°)

\(\theta_{\max }^{*}\) :

Maximum apparent dip angle in the shear direction (°)

φb :

Basic friction angle of the rock joint (°)

δh :

Shear displacement (mm)

δv :

Normal displacement (mm)

τ:

Shear strength (MPa)

τpeak :

Peak shear strength (MPa)

τresidual :

Residual shear strength (MPa)

τpeak,mea :

Measured peak shear strength (MPa)

τpeak,cal :

Calculated peak shear strength by the criterion (MPa)

\(\overline{\sigma }_{\text{ave}}\) :

Average estimation error

σn :

Normal stress (MPa)

σn,crit :

Normal stress at the critical state (MPa)

σt :

Tensile strength (MPa)

i :

Positive integer

m :

Number of samples

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Acknowledgments

The work described herein was performed at the Rock Mechanics and Engineering Centre of Tongji University, with financial support from the National Natural Science Foundation of China via grant nos. 51278378 and 40972178. The authors acknowledge the financial support from the Major State Basic Research Development Program of China (973 Program, no. 2011CB013800). The work was also supported by the Program for Changjiang Scholars and Innovative Research Team in University via grant no. IRT1029. The first author thanks Dr. Jie Zhang of Tongji University for the helpful discussions on the work presented and Yan Ping for the language assistance. We appreciate the anonymous reviewers for their valuable comments and suggestions to improving this manuscript.

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Correspondence to Zhi-Cheng Tang.

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Xia, CC., Tang, ZC., Xiao, WM. et al. New Peak Shear Strength Criterion of Rock Joints Based on Quantified Surface Description. Rock Mech Rock Eng 47, 387–400 (2014). https://doi.org/10.1007/s00603-013-0395-6

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