Rock and Soil Mechanics ›› 2024, Vol. 45 ›› Issue (2): 454-464.doi: 10.16285/j.rsm.2023.0273

• Fundamental Theroy and Experimental Research • Previous Articles     Next Articles

Creep damage model of weak interlayer based on fractional order integral

CAO Jian-jun1, 2, HU Bin1, 2, WANG Ze-qi1, 2, LI Jing1, 2   

  1. 1. Resources and Environmental Engineering, Wuhan University of Science and Technology, Wuhan, Hubei 430081, China; 2. Hubei Key Laboratory for Efficient Utilization and Agglomeration of Metallurgic Mineral Resources, Wuhan University of Science and Technology, Wuhan, Hubei 430081, China
  • Received:2023-03-04 Accepted:2023-07-02 Online:2024-02-11 Published:2024-02-06
  • Supported by:
    This work was supposed by the Key Program of National Natural Science Foundation of China (U1802243) and the Wuhan University of Science and Technology Innovation Team for Cultivation of Major Science and Technology Projects (2018TDX01).

Abstract: The soft interlayer, often considered the “weak link” of slopes, poses a significant threat to slope stability. This study focuses on the Permian carbonaceous shale soft interlayer commonly found in Southwest China. The creep characteristics of the soft interlayer were investigated, and a graded shear creep test was conducted in addition to conventional shear tests to analyze the shear deformation behavior of the soft interlayer comprehensively. The long-term strength of the soft interlayer was determined using the steady-state creep rate method. Building upon the Riemann-Liouville fractional order integral theory and statistical damage theory, an improved model based on the traditional Nishihara model was developed. The accuracy of the model was verified using the adaptive differential evolution algorithm in combination with the weak interlayer shear creep test curve, followed by a parameter sensitivity analysis. The results demonstrate that the improved model adequately describes the three stages of creep in the weak interlayer. The creep curve is influenced by the differential order γ , the shape parameter m, and the proportional parameter F0. Parameter m reflects the brittle characteristics of the soft interlayer, while parameter F0 characterizes its physical and mechanical strength. The research results can provide a theoretical basis for disaster prevention monitoring and stability analysis of slopes with weak interlayer.

Key words: weak interlayer, fractional order integrals, creep model, parameter identification, sensitivity analysis

CLC Number: 

  • TU 45
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