岩土力学 ›› 2026, Vol. 47 ›› Issue (3): 1031-1040.doi: 10.16285/j.rsm.2025.0245CSTR: 32223.14.j.rsm.2025.0245

• 岩土工程研究 • 上一篇    下一篇

剪切带非对称扩展下的海底边坡稳定性分析方法

武广瑶,朱志鹏,王栋   

  1. 中国海洋大学 海底建设与保护山东省工程研究中心,山东 青岛 266100
  • 收稿日期:2025-03-09 接受日期:2025-07-07 出版日期:2026-03-17 发布日期:2026-03-24
  • 通讯作者: 王栋,男,1975年生,博士,教授,主要从事海洋岩土工程方面研究。E-mail: dongwang@ouc.edu.cn
  • 作者简介:武广瑶,女,2000年生,博士研究生,主要从事海底滑坡方面研究。E-mail: wuguangyao@stu.ouc.edu.cn
  • 基金资助:
    国家自然科学基金项目(No.42025702,No.52394251)。

Stability analysis of submarine slopes with asymmetric shear band propagation

WU Guang-yao, ZHU Zhi-peng, WANG Dong   

  1. Shandong Engineering Research Center of Marine Exploration and Conservation, Ocean University of China, Qingdao, Shandong 266100, China
  • Received:2025-03-09 Accepted:2025-07-07 Online:2026-03-17 Published:2026-03-24
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (42025702, 52394251).

摘要: 海底滑坡常出现在坡度不超过5º的黏土质缓坡,常规极限平衡法很难再现这种现象,而剪切带扩展法由黏性土的应变软化出发,提出了缓坡失稳的合理解释。以往剪切带扩展法几乎都是针对平直或对称S形边坡,将剪切带的对称扩展简化为单向问题,但实际边坡形态多为非对称。提出了剪切带非对称扩展分析方法,根据潜在滑动面的整体变形协调条件,计算扩展过程中剪应力等变量的演变,评估边坡稳定性。以非对称的高斯型边坡为例,探究局部扰动后的边坡渐进破坏过程,发现当剪切带扩展长度超过临界值时,将诱发灾难性失稳。边坡曲率变化越小,失稳时潜在滑动面最陡处的临界自重剪应力越接近剪切带土体的不排水强度峰值,进而提出了简化失稳准则,并通过有限元模拟验证了其普适性和准确性。以瑞士St. Niklausen滑坡为例,对比了不同分析方法的预测效果。极限平衡法和将边坡近似为对称形状的传统剪切带扩展方法,高估了边坡稳定性。提出的非对称分析方法能够合理再现St. Niklausen滑坡的发生,预测的安全系数和剪切带位置与有限元结果接近。构建的简化失稳准则能够快速给出偏于保守的评估结果。

关键词: 海底滑坡, 渐进破坏, 应变软化, 剪切带扩展, 稳定性分析

Abstract: Submarine landslides often occur on gentle cohesive slopes with inclinations of less than 5°, which cannot be adequately reproduced using traditional limit equilibrium methods. The shear band propagation method, considering the strain-softening behavior of cohesive soils, provides a rational explanation for such failures. Previous shear band propagation methods mostly focused on planar or symmetrical S-shaped slopes, where the symmetric propagation of shear bands is simplified as a unidirectional problem. However, most natural slopes are characterized by asymmetric profiles. A theoretical method for asymmetric shear band propagation is proposed, where the evolution of shear stress and related variables is solved based on deformation compatibility along the entire slip surface to assess slope stability. Using the asymmetric Gaussian slope as an example, the progressive failure process triggered by local disturbances is investigated. The results show that when the shear band length exceeds a critical value, catastrophic failure occurs. As the curvature variation of the slope decreases, the critical gravity shear stress at the steepest point of the potential slip surface approaches the peak undrained shear strength of soils. Based on these findings, a simplified failure criterion is proposed and its general applicability and accuracy are verified through finite element analysis. A case study of the St. Niklausen landslide in Switzerland is conducted to evaluate the prediction performance/predictive capability of different methods. Limit equilibrium methods and conventional symmetric shear band propagation methods that approximate the slope as a symmetric shape overestimate slope stability. The proposed asymmetric analysis method can reasonably reproduce the occurrence of the St. Niklausen slide, with predicted safety factors and shear band locations closely matching finite element results. The developed simplified failure criterion provides quick stability evaluations with a conservative bias.

Key words: submarine landslide, progressive failure, strain-softening, shear band propagation, stability analysis

中图分类号: TU441
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