4.6 Article

A strain-based fatigue damage model for naturally fractured marble subjected to freeze-thaw and uniaxial cyclic loads

Journal

INTERNATIONAL JOURNAL OF DAMAGE MECHANICS
Volume 30, Issue 10, Pages 1594-1616

Publisher

SAGE PUBLICATIONS LTD
DOI: 10.1177/10567895211021629

Keywords

Freeze-thaw cycle; natural fracture; cyclic loads; damage evolution model; CT scanning

Funding

  1. Beijing Natural Science Foundation [8202033]
  2. National key technologies Research and Development program [2018YFC0808402]
  3. Fundamental Research Funds for the Central Universities [FRF-TP-20-004A2]
  4. National Natural Science Foundation of China [51774021]

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This study aims to investigate the fatigue damage evolution of rock caused by volumetric deformation from freeze-thaw and cyclic loads, as well as the influence of natural fractures on rock damage characteristics. Experimental results show that frost heaving force acting on natural fractures leads to volume changes in rock, and the damage variable expressed by volumetric strain has a linear relationship with freeze-thaw cycles. Marble exposed to cyclic loads exhibits a two-stage pattern in axial, lateral, and volumetric strain.
The naturally fractured rock in the open pit slope is susceptible to irreversible damage caused by fatigue loads related to freeze-thaw weathering, blasting vibration, earthquakes and tramcar traffic. To ensure the safety of rock mass and reveal how natural fracture affects the damage modelling characteristics is of great concern. Hence, this work aims at investigating the fatigue damage evolution of rock from volumetric deformation caused by F-T and cyclic loads. The rock structural deterioration and damage accumulation were investigated as well as the stimulated natural fracture pattern. Results show the frost heaving force acted on natural fracture results in the rock volumetric changes. The damage variable expressed by volumetric strain presents a linear relationship with freeze-thaw cycles. In addition, the axial, lateral and volumetric strain of marble exposed to cyclic loads present a two-stage pattern, they first increase quickly and then get to steady and last for a long time. A new fatigue damage model was established by considering the freeze-thaw damage and mechanical damage simultaneously. The proposed coupling damage model can well describe rock damage accumulation. Moreover, the CT images further reveal the influence of the natural fracture on rock volumetric deformation and the final damage accumulation. It is suggested that the opening-mode natural fractures contribute a lot to rock freeze-thaw deformation and fatigue deformation.

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