4.6 Article

Energy-driven damage evolution and instability in fissure-cavity-contained granite induced by freeze-thaw and multistage increasing-amplitude cyclic (F-T-MSIAC) loads

期刊

INTERNATIONAL JOURNAL OF DAMAGE MECHANICS
卷 32, 期 3, 页码 362-386

出版社

SAGE PUBLICATIONS LTD
DOI: 10.1177/10567895221144073

关键词

Hollow-cylinder granite; cyclic loads; energy conversion; damage evolution; CT images

向作者/读者索取更多资源

This study investigates the damage and fracture evolution of rock containing fissures and hollow hole under freeze-thaw and cyclic loads. The results show that the volumetric deformation of rock decreases with increasing freeze-thaw cycles, and both elastic strain energy and dissipated strain energy decrease as well. A coupling damage evolution model considering freezing-thaw and mechanical damage is proposed.
Rock damage and fracture is energy-driven, the energy conversion characteristics for the pre-flawed rock under static or fatigue loading conditions have been well widely studied. However, energy mechanism of rock containing fissures and hollow hole exposed to coupled freeze-thaw and cyclic loads is not well understood. In this work, damage and fracture evolution of pre-flawed hollow-cylinder granite specimens induced by freeze-thaw and multistage increasing-amplitude cyclic (F-T-MSIAC) loads were investigated using energy analysis. Testing results show that the volumetric deformation of rock is affected by the previous freeze-thaw cycles. Rock volumetric deformation decreases with increasing freeze-thaw cycle. The elastic strain energy and dissipated strain energy both decreases with increasing freeze-thaw cycles. When rocks undergo relatively small freeze-thaw cycles, a large amount of energy is consumed to drive crack propagation and cavity collapse. A coupling damage evolution model considering the freezing-thaw and mechanical damage was proposed. The model fits well to the two-stage and three-stage damage accumulation pattern. Two-dimensional CT images reveal different fracture network morphology and the effect of freeze-thaw weathering on crack coalescence. The results show that rock fracture is easy to occur under high freeze-thaw cycles, and less energy is required to communicate the fissures and hollow hole.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.6
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据