4.7 Article

Three-dimensional upper-bound analysis of rock slopes subjected to seepage forces based on Hoek-Brown failure criterion

Journal

COMPUTERS AND GEOTECHNICS
Volume 138, Issue -, Pages -

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.compgeo.2021.104310

Keywords

Limit analysis; 3D slope; Seepage force; Hoek-Brown failure criterion; Stability analysis

Funding

  1. Fundamental Research Funds for the Central Universities of Central South University [2021zzts0768]

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The paper presents a method for analyzing the stability of rock slopes in three dimensions, solving the hydraulic head distribution and calculating the seepage forces under steady state hydraulic conditions using numerical methods. The approach is validated through parametric analysis, showing that the safety factor increases with certain parameters but decreases with slope angle and aspect ratio increases.
Three-dimensional upper-bound analysis of rock slopes subjected to seepage flows is a classical problem in geotechnical engineering. However, it is difficult to obtain a rigorous upper-bound solution of the safety factor of slopes when seepage flows are involved. In order to address this problem, the three-dimensional (3D) hydraulic head distributions inside a slope under steady state hydraulic conditions are solved numerically. The obtained numerical hydraulic head distributions are further employed to compute the seepage forces applying to the 3D discretized rotational failure mechanism to assess the stability of a rock slope. The Hoek-Brown yield criterion is employed to characterize the failure of rock masses. The generalized tangential technique is employed to formulate the problem as a classical optimization problem. The particle swarm optimization algorithm combined with the Nelder-Mead simplex algorithm is used to search for the best solutions of slope safety factor. The proposed approach is validated by comparing with 2D plane strain analysis results in the literature. Parametric analysis shows that the safety factor increases as mi or GSI increases, but decreases with the increase of the slope angle beta and B/H. It is also found that the 3D influence is significant for B/H smaller than 10, beyond which it becomes negligible. The computational results in the form of design tables are presented for practical use in rock engineering.

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