Model Test Study on the Anisotropic Characteristics of Columnar Jointed Rock Mass
Abstract
:1. Introduction
2. Structural Characteristics of the CJRM
3. Model Tests
3.1. Similar Material and Model Size
3.2. Manufacturing Process of Specimens
3.3. Testing Equipment and Procedure
4. Test Results
4.1. Deformation and Strength Behavior
4.2. Failure Modes and Mechanisms
- Mode I:
- Splitting failure through joint planes. This mode occurs in the 4P- and 5P-CJRM specimens with the dip directions of 0, 15, 75 and 90° and in all the 6P-CJRM specimens. As observed from Figure 9a, the cracks initiate at the column material and propagate in the vertical direction. Eventually, failure surfaces passing through the joint planes appear on the specimen. Therefore, no sliding along the joint plane is observed, and the damage of the specimen is tensile failure.
- Mode II:
- Sliding failure along persistent joint plane. This mode occurs in the 4P-CJRM specimens with the dip directions of 30, 45 and 60° and in the 5P-CJRM specimen with the dip direction of 30°. The cracks initiate at the persistent joint plane and propagate along the persistent joint (Figure 9b). Eventually, sliding failure occurs along the persistent joint plane because the shear stress acting on the joint plane is greater than its shear strength.
- Mode III:
- Mixed failure along joint plane. This mode occurs in the 5P-CJRM specimens with the dip directions of 45 and 60°. The cracks initiate at the interlocking joints on the top of the pentagon, and appear at the joints on the sides of the pentagon under the further load (Figure 9c). Eventually, the cracks at the two locations connect and form a failure surface. The initial cracks are caused by tension because the angle between the joint and the load direction is small. The further load makes the columns slide along the sides of the pentagon, and the lateral deformation of the specimen accelerates the propagation of the cracks at the interlocking joints. Therefore, the failure mode of the specimen is mixed failure along the joint plane.
5. Discussion
5.1. Anisotropic Degrees in Horizontal Plane
5.2. Anisotropic Characteristics of the Three CJRM Models
5.3. Theoretical Prediction of Strength and Deformation
6. Conclusions
- (1)
- The differences between the strength and deformation behaviors of the three CJRM models were mainly caused by the structural features of these three models. The curves of 4P-CJRM were symmetrical, while the curves of 6P-CJRM were approximately straight. For 6P-CJRM, the variation curves combined the characteristics of the above two models.
- (2)
- Three typical failure modes of the CJRM specimens with different dip directions α were summarized, including the splitting failure through joint planes, the sliding failure along a persistent joint plane and the mixed failure along a joint plane.
- (3)
- The anisotropy ratio was introduced to classify the anisotropic degrees of the three CJRM models. The anisotropic degrees of the 4P-, 5P- and 6P-CJRM models in the horizontal plane were medium, low and low, respectively.
- (4)
- The anisotropic characteristics of the three CJRM models were described by placing the test results in the polar coordinates. The curves of the 4P- and 5P-CJRM models in the horizontal plane were all an axisymmetric diagram resembling a gyro, which indicated their orthotropy. The curves of the 6P-CJRM were approximately circular, which revealed its quasi-transverse isotropy.
- (5)
- A simple empirical expression was adopted to estimate the strength and deformation of the CJRM, and the derived equations were used in the Baihetan CJRM. The calculated values were all within the ranges of the existing research results, which indicates that the derived empirical equations are valuable for related engineering applications.
Author Contributions
Funding
Acknowledgments
Conflicts of Interest
References
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Material | Density (g/cm3) | Compressive Strength (MPa) | Elastic Modulus (GPa) | Poisson’s Ratio | Cohesion (MPa) | Friction Angle (°) |
---|---|---|---|---|---|---|
Intact basalt 1 | 2.83–2.93 | 47.7–255.0 | 30.0–86.6 | 0.17–0.26 | 10.0–13.0 | 45–50 |
Rock-like material | 1.17 | 6.58 | 1.24 | 0.19 | 1.37 | 51.3 |
Shape of Columns | Dip Direction (°) | Elastic Modulus (GPa) | UCS (MPa) |
---|---|---|---|
Quadrangular prism | 0 | 0.429 | 3.193 |
15 | 0.311 | 2.052 | |
30 | 0.258 | 1.427 | |
45 | 0.214 | 1.396 | |
60 | 0.258 | 1.427 | |
75 | 0.311 | 2.052 | |
90 | 0.429 | 3.193 | |
Pentagonal prism | 0 | 0.282 | 2.376 |
15 | 0.267 | 1.973 | |
30 | 0.229 | 1.495 | |
45 | 0.196 | 1.267 | |
60 | 0.237 | 1.384 | |
75 | 0.262 | 1.962 | |
90 | 0.275 | 2.210 | |
Hexagonal prism | 0 | 0.255 | 2.092 |
15 | 0.240 | 1.937 | |
30 | 0.243 | 1.892 | |
45 | 0.242 | 1.933 | |
60 | 0.255 | 2.092 | |
75 | 0.240 | 1.937 | |
90 | 0.243 | 1.892 |
Normalized UCS σcr | Normalized Elastic Modulus Ecr |
---|---|
σcr = 0.388 − 0.155cos [2(45° − α)] (0° ≤ α < 45°) σcr = 0.370 − 0.137cos[2 (45° − α)] (45° ≤ α ≤ 90°) | Ecr = 0.260 − 0.084cos[2(45° − α)] (0° ≤ α < 45°) Ecr = 0.256 − 0.080cos[2(45° − α)] (45° ≤ α ≤ 90°) |
Result | Normalized UCS σcr | Normalized Elastic Modulus Ecr |
---|---|---|
Calculated result | 0.24 | 0.181 |
Existing research result 2 | 0.1430.536 | 0.157–0.552 |
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Zhu, Z.; Que, X.; Niu, Z.; Lu, W. Model Test Study on the Anisotropic Characteristics of Columnar Jointed Rock Mass. Symmetry 2020, 12, 1528. https://doi.org/10.3390/sym12091528
Zhu Z, Que X, Niu Z, Lu W. Model Test Study on the Anisotropic Characteristics of Columnar Jointed Rock Mass. Symmetry. 2020; 12(9):1528. https://doi.org/10.3390/sym12091528
Chicago/Turabian StyleZhu, Zhende, Xiangcheng Que, Zihao Niu, and Wenbin Lu. 2020. "Model Test Study on the Anisotropic Characteristics of Columnar Jointed Rock Mass" Symmetry 12, no. 9: 1528. https://doi.org/10.3390/sym12091528