Abstract

Rockslides along a stepped failure surface have characteristics of stepped deformation characteristic and it is difficult to predict the failure time. In this study, the deformation characteristics and disaster prediction model of the Fengning granite rockslide were analyzed based on field surveys and monitoring data. To evaluate the stability, the shear strength parameters of the sliding surface were determined based on the back-propagation neural network and three-dimensional discrete element numerical method. Through the correlation analysis of deformation monitoring results with rainfall and blasting, it is shown that the landslide was triggered by excavation, rainfall, and blasting vibrations. The landslide displacement prediction model was established by using long short-term memory neural network (LSTM) based on the monitoring data, and the prediction results are compared with those using the BP model, SVM model and ARMA model. Results show that the LSTM model has strong advantages and good reliability for the stepped landslide deformation with short-term influence, and the predicted LSTM values were very consistent with the measured values, with a correlation coefficient of 0.977. Combined with the distribution characteristics of joints, the damage influence scope of the landslide was simulated by three-dimensional discrete element, which provides decision-making basis for disaster warning after slope instability. The method proposed in this paper can provide references for early warning and treatment of geological disasters.

Highlights

  • Excavation often causes slope damage in areas with complex geological conditions.This results in huge casualties, property losses, and construction delays [1]

  • Different batch sizes affect the Predictions of landslide deformation trends and influence scope are important bases accuracy of the model

  • long short-term memory neural network (LSTM) and numerical method which indicates that the prediction gradually

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Summary

Introduction

Excavation often causes slope damage in areas with complex geological conditions. This results in huge casualties, property losses, and construction delays [1]. The failure surface is often formed by a combination of steeply and gently inclined fissures. The combination of steeply and gently inclined fissures has an important influence on the deformation, failure evolution, and stability of the slope [2]. Combined with steep dip fractures, bed-like rock mass structures readily form resulting in a landslide failure surface with a combination of steep and gentle fractures. This stepped failure mode is more common in western China

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