4.6 Article

Failure of Rock Slope with Heterogeneous Locked Patches: Insights from Numerical Modelling

Journal

APPLIED SCIENCES-BASEL
Volume 11, Issue 18, Pages -

Publisher

MDPI
DOI: 10.3390/app11188585

Keywords

rock slope; locked patch; shear strength; mechanical model

Funding

  1. National Key Research and Development Plan [2018YFC1505301]

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This study investigates the impact of naturally heterogeneous locked patches of different properties on rock slope stability. It is found that rock homogeneity affects the failure mode, and the length and strength of locked patches have a significant influence on shear strength and displacement. Additionally, the sequence of failure is affected by the relative positions of the locked patches.
Rock slope stability is commonly dominated by locked patches along a potential slip surface. How naturally heterogeneous locked patches of different properties affect the rock slope stability remains enigmatic. Here, we simulate a rock slope with two locked patches subjected to shear loading through a self-developed software, rock failure process analysis (RFPA). In the finite element method (FEM)-based code, the inherent heterogeneity of rock is quantified by the classic Weibull distribution, and the constitutive relationship of the meso-scale element is formulated by the statistical damage theory. The effects of mechanical and geometrical properties of the locked patches on the stability of the simulated rock slope are systematically studied. We find that the rock homogeneity modulates the failure mode of the rock slope. As the homogeneity degree is elevated, the failure of the locked patch transits from the locked patch itself to both the interfaces between the locked patched and the slide body and the bedrock, and then to the bedrock. The analysis of variance shows that length and strength of locked patch affect most shear strength and the peak shear displacement of the rock slope. Most of the rock slopes exhibit similar failure modes where the macroscopic cracks mainly concentrate on the interfaces between the locked patch and the bedrock and the slide body, respectively, and the acoustic events become intensive after one of the locked patches is damaged. The locked patches are failed sequentially, and the sequence is apparently affected by their relative positions. The numerically reproduced failure mode of the rock slope with locked patches of different geometrical and mechanical properties are consistent with the laboratory observations. We also propose a simple spring-slider model to elucidate the failure process of the rock slope with locked patches.

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