2022
DOI: 10.1111/ffe.13760
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On the effect of confining pressure on fatigue failure of block‐in‐matrix soils exposed to multistage cyclic triaxial loads

Abstract: This paper discusses the multi-level cyclic triaxial testing of bimsoils (block-inmatrix soils), which are chaotic, mechanically and/or spatially heterogeneous geological masses in geotechnical construction. The cyclic triaxial tests simulate the behavior of bimsoil material under varying number of passing vehicle wheels. It is found that the applied confining pressure alters the stress state of the tested bimsoil and a transmission from strain softening to strain hardening occurs. The bimsoil deformation, str… Show more

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Cited by 25 publications
(23 citation statements)
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“…Globally, there are more than a dozen major methods and hundreds of instruments up to now. The major methods include hydraulic fracturing, stress relief, stress recovery, borehole collapse, acoustic emission, and geophysical method [6][7][8][9][10][11][12][13][14][15][16][17][18][19][20].…”
Section: Major Existing Methods For Measuring In Situ Stress and Thei...mentioning
confidence: 99%
“…Globally, there are more than a dozen major methods and hundreds of instruments up to now. The major methods include hydraulic fracturing, stress relief, stress recovery, borehole collapse, acoustic emission, and geophysical method [6][7][8][9][10][11][12][13][14][15][16][17][18][19][20].…”
Section: Major Existing Methods For Measuring In Situ Stress and Thei...mentioning
confidence: 99%
“…Therefore, the landslide rock mass and internal structure can be viewed as a whole when judging the instability mechanism of the whole system. According to the variation trend of each data factor at different time nodes and the above-mentioned deformation characteristics, the system deformation can be divided into four stages: initial deformation stage I, uniform deformation stage II, accelerated deformation stage III (divided into the first accelerated deformation stage (1) and the second accelerated deformation stage (2)), and residual deformation stage IV [34]. In stage I, under the influence of external force, the soil stress behind the pile begins to rise and is transferred to the micropile.…”
Section: Comprehensive Analysis Of Multisource Datamentioning
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%