4.3 Article

Simulation on heterogeneous rocks with a flaw using grain-based discrete-element method

Journal

GEOTECHNIQUE LETTERS
Volume 11, Issue 1, Pages -

Publisher

ICE PUBLISHING
DOI: 10.1680/jgele.20.00083

Keywords

discrete-element modelling; mineralogy; rocks/rock mechanics

Funding

  1. National Key R&D Program of China [2020YFA0711802]
  2. National Natural Science Foundation of China [51809137, 41525009]
  3. Natural Science Foundation of Jiangsu Province [BK 20180480]

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In this study, the effect of mineral microstructure on crack growth and mechanical properties of heterogeneous rocks with a single pre-existing flaw under uniaxial compression was investigated using the discrete-element method combined with a grain-based model. The results show that characteristic stresses increase with the inclination angle, and intergranular cracks initiate prior to intragranular cracks. Ultimately, the numerical simulations of failure patterns align well with experimental results, revealing a combination of intragranular and intergranular cracks at the grain scale.
To take into consideration the effect of mineral microstructure on crack growth and mechanical properties of heterogeneous rocks containing a single pre-existing flaw under uniaxial compression, the discrete-element method in combination with the grain-based model was adopted in this study. The results indicate that the characteristic stresses - that is, crack initiation stress, crack damage stress and peak strength, generally increase with respect to the inclination angle. The normalised crack initiation stress increases with the increasing angle, while the normalised crack damage stress has no pronounced change. Additionally, the variation of inclination angles has little influence on the grain-scale crack growth. The initiation of intergranular cracks is prior to the intragranular cracks, and the proportion of intragranular cracks is slightly greater than intergranular cracks at the peak failure moment. The ultimate failure patterns obtained by numerical simulations agree well with the experimental results, revealing the cracks generated from the pre-existing flaw consist of intragranular and intergranular cracks at the grain scale.

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