2022
DOI: 10.1016/j.ijfatigue.2022.107014
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Macro-meso fatigue failure of bimrocks with various block content subjected to multistage fatigue triaxial loads

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Cited by 38 publications
(28 citation statements)
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“…Frost heaving force is easily formed in the interfaces, pores, and microcracks, which leads to damage propagation, aperture growth and length increase, and the bimrock structure deterioration. Besides, in geotechnical engineering, for example, mining and civil engineering, disturbed stress is inevitable in the process of rock mass construction; 25–28 the disturbed stress conditions improve the reactivation of fault bands. Although large number of attempts have been carried out on rock fracture and instability behaviors under cyclic or fatigue loads, most of the investigations are focused on fissure‐contained 29,30 or cavity‐contained rock mass 31–33 .…”
Section: Introductionmentioning
confidence: 99%
“…Frost heaving force is easily formed in the interfaces, pores, and microcracks, which leads to damage propagation, aperture growth and length increase, and the bimrock structure deterioration. Besides, in geotechnical engineering, for example, mining and civil engineering, disturbed stress is inevitable in the process of rock mass construction; 25–28 the disturbed stress conditions improve the reactivation of fault bands. Although large number of attempts have been carried out on rock fracture and instability behaviors under cyclic or fatigue loads, most of the investigations are focused on fissure‐contained 29,30 or cavity‐contained rock mass 31–33 .…”
Section: Introductionmentioning
confidence: 99%
“…Here, some new terminologies are used for bimrocks, such as block-in-matrix-soils (bimsoils), 8,9 rock and soil aggregation (RSA), 10 and soil and rock mixture (SRM), 11,12 such as mélanges, coarse pyroclastic rocks, breccias, colluviums and alluviums, fault rocks, and conglomerates, etc. The static mechanical behaviors of bimrock have been widely investigated by laboratory compression tests 13 or shear tests, 14 field shear tests, 15,16 numerical tests, 17 and so forth. For the fault rocks, some scholars conducted laboratory tests to study its strength and deformation characteristics.…”
Section: Introductionmentioning
confidence: 99%
“…The threedimensional stress is the occurrence condition of the fractured rock mass, and the fracture dip angle is the geometric state of the fracture itself. These two aspects have mutual influence on the slurry migration in the fracture and are a pair of coupling factors [39][40][41][42][43][44]. In a word, the slurry diffusion in the fractured rock body needs to consider the slurry diffusion mechanism in the fractured rock body with different dip angles under the three-dimensional stress environment, which is the research direction that meets the needs of the project.…”
Section: Introductionmentioning
confidence: 99%