4.7 Article

Spatial variability effect of internal friction angle on the post-failure behavior of landslides using a random and non-Newtonian fluid based SPH method

Journal

GEOSCIENCE FRONTIERS
Volume 11, Issue 4, Pages 1107-1121

Publisher

CHINA UNIV GEOSCIENCES, BEIJING
DOI: 10.1016/j.gsf.2020.02.003

Keywords

Landslides; Spatial variability; Random field; Smoothed particle hydrodynamics; Monte Carlo simulation; Post-failure behavior

Funding

  1. Natural Science Foundation of China (NSFC) [51808192, 51879091, 41630638]
  2. Natural Science Foundation of Jiangsu Province [BK20170887]
  3. China Postdoctoral Science Foundation [2017M611673, 2018T110432]

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This study proposed a random Smoothed Particle Hydrodynamics method for analyzing the post-failure behavior of landslides, which is based on the Karhunen-Loeve (K-L) expansion, the non-Newtonian fluid model, and the OpenMP parallel framework. Then, the applicability of this method was validated by comparing the generated random field with theoretical result and by simulating the post-failure process of an actual landslide. Thereafter, an illustrative landslide example was created and simulated to obtain the spatial variability effect of internal friction angle on the post-failure behavior of landslides under different coefficients of variation (COVs) and correlation lengths (CLs). As a conclusion, the reinforcement with materials of a larger friction angle can reduce the runout distance and impact the force of a landslide. As the increase of COV, the distribution range of influence zones also increases, which indicates that the deviation of influence zones becomes large. In addition, the correlation length in Monte Carlo simulations should not be too small, otherwise the variation range of influence zones will be underestimated.

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