Skip to main content
Log in

Cracking Processes and Coalescence Modes in Rock-Like Specimens with Two Parallel Pre-existing Cracks

  • Original Paper
  • Published:
Rock Mechanics and Rock Engineering Aims and scope Submit manuscript

Abstract

The cracks in a rock tend to initiate, propagate, and coalesce under loading. Based on the digital image correlation (DIC) method, uniaxial compression tests are carried out on rock-like specimens with various arrangements of two parallel cracks. The full-field strain and failure features of the rock-like materials are observed and analysis by a self-developed code. Two process zones are defined according to the differences between the shear strain field and the tensile strain field: a shear process zone and a tensile process zone. The following results are obtained in this study. (1) Three coalescence modes can be observed using the DIC method: a shear coalescence mode, a tensile coalescence mode, and a mixed coalescence mode. (2) At the microscopic level, the bridge angle and crack arrangement affect the formation of the process zone; at the macroscopic level, they determine the crack propagation path and the failure mode. (3) The peak strength of the rock-like specimen is related to the crack inclination angle and the bridge angle. (4) Numerical modeling by the expanded distinct element method and the strain strength criterion simulates the different coalescence modes of the experimental study efficiently.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11
Fig. 12
Fig. 13
Fig. 14
Fig. 15
Fig. 16
Fig. 17
Fig. 18
Fig. 19
Fig. 20
Fig. 21
Fig. 22
Fig. 23
Fig. 24

Similar content being viewed by others

Abbreviations

α :

Crack inclination angle

β :

Bridge angle

\({\varepsilon _t}\) :

Critical tensile strain

\({\gamma _{xy{\text{cri}}}}\) :

Critical shear strain

\({\sigma _t}\) :

Critical tensile strength

\({\sigma _{\text{c}}}\) :

Critical compressive strength

\({\sigma _1},{\sigma _3}\) :

Maximum and minimum principal stresses, respectively

\(\nu\) :

Poisson’s ratio

\(\varphi\) :

Internal friction angle

c :

Cohesion

C :

Correlation coefficient

E :

Young’s modulus

G :

Shear modulus

\({f_{1m}},{f_{2m}}\) :

Average gray values of the reference and deformed images, respectively

\({f_1}(x,y),{f_2}(x',y')\) :

Gray-level values for the reference and deformed images, respectively

\({f_{\text{t}}},{f_{\text{s}}}\) :

Judgement factors of the tensile and shear cracks, respectively

BPM:

Bonded-particle model

DDM:

Displacement discontinuity method

DEM:

Discrete element method

DIC:

Digital image correlation

EDEM:

Expanded distinct element method

LEFM:

Linear elastic fracture mechanics

PFC:

Particle flow code

SIF:

Stress intensity factor

SPZ:

Shear process zone

TPZ:

Tensile process zone

UDEC:

Universal distinct element code

References

Download references

Acknowledgements

The authors would like to acknowledge the financial support of the National Key R&D Program of China (no. 2017YFC0806000), the National Natural Science Foundation of China (nos. 41202193 and 41572262), the Innovation Program of the Shanghai Municipal Education Commission (no. 15ZZ016), and the Shanghai Rising-Star Program (no. 17QC1400600).

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Cheng Zhao.

Ethics declarations

Conflict of interest

No potential conflicts of interests were reported by the authors.

Additional information

Publisher’s Note

Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Zhao, C., Zhou, Y.m., Zhao, C.f. et al. Cracking Processes and Coalescence Modes in Rock-Like Specimens with Two Parallel Pre-existing Cracks. Rock Mech Rock Eng 51, 3377–3393 (2018). https://doi.org/10.1007/s00603-018-1525-y

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00603-018-1525-y

Keywords

Navigation