4.7 Article

Volumetric deformation and damage evolution of Tibet interbedded skarn under multistage constant-amplitude-cyclic loading

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.ijrmms.2022.105066

关键词

Interbedded skarn; Anisotropy; MCAC loads; Volumetric deformation; Damage evolution

资金

  1. National Natural Science Foundation of China (NSFC) [41941018, 52104125, 42007256]
  2. National Key Technologies Research & Development program [2018YFC0808402]
  3. State Key Laboratory for Geo-Mechanics and Deep Underground Engineering, China University ofMining & Technology, Beijing [SKLGDUEK2133]
  4. Fundamental Research Funds for the Central Universities

向作者/读者索取更多资源

Multistage constant-amplitude cyclic loading experiments were conducted on Tibet interbedded skarn to investigate the fatigue mechanical behavior of the rock. The results showed that the volumetric deformation and damage evolution of the skarn were influenced by the interbed structure. A new damage evolution model was proposed and different fracture mechanisms were identified through macroscopic failure morphology analysis.
Multistage constant-amplitude-cyclic (MCAC) loading experiments were conducted on Tibet interbedded skarn to investigate and characterize fatigue mechanical behavior of the tested rock. Rock volumetric deformation, stiffness change, and fatigue damage evolution were analyzed along with the macroscopic failure morphology. The experimental results demonstrated that the volumetric deformation of the tested skarn was influenced by the interbed structure. Rock damage presented a two-stage pattern. The rock damage increased quickly at the beginning and subsequently became steady for long periods of time within a cyclic loading stage. A new damage evolution model was proposed on the basis of axial strain. Macroscopic failure morphology analysis revealed different fracture mechanisms, combining a tension-splitting mode, shear-sliding, and mixed shear-tension. In this study, the understanding of the anisotropic mechanical properties of interbedded skarn was highlighted, and this could contribute to the ability to predict the stabilities of rock engineering structures.

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