4.7 Article

Effect of Heterogeneity on the Extension of Ubiquitiformal Cracks in Rock Materials

期刊

FRACTAL AND FRACTIONAL
卷 6, 期 6, 页码 -

出版社

MDPI
DOI: 10.3390/fractalfract6060317

关键词

ubiquitiformal fracture energy; ubiquitiformal complexity; heterogeneity; homogeneity; Brazilian splitting strength

资金

  1. National Natural Science Foundation of China [11872300, 11572244]
  2. Natural Science Foundation of Shaanxi Province, China [2021JQ-463, 2021JZ-47]
  3. Youth Innovation Team of Shaanxi Universities

向作者/读者索取更多资源

Fracture energy, an important parameter for characterizing the fracture properties of materials, has been extensively studied. This paper focuses on ubiquitiform fracture energy and investigates the crack extension of slate and granite using the Brazilian splitting test. The complexity and ubiquitiform fracture energy of rock material are obtained, and the effect of heterogeneity on ubiquitiform cracks is simulated. The results show the range of complexity for slate and granite and the influence of heterogeneity on the Brazilian splitting strength.
Fracture energy, as an important characteristic parameter of the fracture properties of materials, has been extensively studied by scholars. However, less research has been carried out on ubiquitiformal fracture energy and the main method used by scholars is the uniaxial tensile test. In this paper, based on previous research, the first Brazilian splitting test was used to study the ubiquitiformal crack extension of slate and granite, and the complexity and ubiquitiformal fracture energy of rock material were obtained. The heterogeneity of the material was then characterized by the Weibull statistical distribution, and the cohesive model is applied to the ABAQUS numerical software to simulate the effect of heterogeneity on the characteristics of ubiquitiformal cracks. The results demonstrate that the ubiquitiformal complexity of slate ranges from 1.54 to 1.60, and that of granite ranges from 1.58 to 1.62. The mean squared deviations of the slate and granite ubiquitiformal fracture energy are the smallest compared with the other fracture energies, which are 0.038 and 0.037, respectively. When the homogeneity of the heterogeneous model is less than 1.5, its heterogeneity has a greater influence on the Brazilian splitting strength, and the heterogeneity of the rock is obvious. However, when the homogeneity is greater than five, the effect on the Brazilian splitting strength is much less, and the Brazilian splitting strength tends to be the average strength. Therefore, it is particularly important to study the fracture problem of cracks from the nature of the material structure by combining the macroscopic and mesoscopic views through the ubiquitiform theory.

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