土工基础 ›› 2026, Vol. 40 ›› Issue (4): 598-602.

• 工程实录 • 上一篇    下一篇

地震作用下边坡稳定性分析及加固方法研究

赵阳1,吴恺2   

  1. (1.上海市徐汇区建设工程质量监督站,上海 200233;2.中亿丰建设集团股份有限公司,江苏苏 215131)
  • 收稿日期:2024-06-13 修回日期:2024-07-05 出版日期:2026-08-30 发布日期:2026-08-26
  • 作者简介:赵阳(1997-),男,硕士,助理工程师,研究方向为工程建设质量监督。

Stability Analysis and Reinforcement Methods of a Slope under Earthquake

ZHAO Yang1, WU Kai2   

  1. (1.Xuhui District Construction Quality and Quantity Supervision Station, Shanghai 200233;
    2.Zhongyifeng Construction Group Co. Ltd., Suzhou 215131)
  • Received:2024-06-13 Revised:2024-07-05 Online:2026-08-30 Published:2026-08-26

摘要: 边坡稳定性分析是岩土工程中非常重要的课题,而地震是边坡失稳的最大诱因之一。地震作用下边坡稳定性及加固方法的研究对地震诱发滑坡灾害的防治具有现实意义。以一层状边坡为模型,采用有限元强度折减法对该边坡进行稳定性分析,并结合拟静力法进行了地震分析。针对地震作用下层状边坡的破坏特征,设计了格构锚杆加固方案对边坡进行加固,分析了格构锚杆对自然状态和地震作用下边坡的加固效果及其对应力场、位移场和安全系数的影响。结果显示,格构锚杆显著提高了自然状态以及地震作用下边坡的安全系数,格构锚杆对边坡有很好的加固效果。地震作用下层状边坡的破坏滑移面较大,最大位移出现在坡脚处。

关键词: 强度折减法, 边坡稳定性, 地震作用, 安全系数, 边坡加固

Abstract: Slope stability assessment is a fundamental issue in geotechnical engineering, with earthquakes recognized as one of the most critical triggers of slope failure. Consequently, understanding the seismic stability of slopes and developing effective reinforcement strategies is essential for mitigating earthquake-induced landslide hazards. In this study, a layered slope model is analyzed using the finite-element strength-reduction method to evaluate baseline stability, while seismic effects are examined through the pseudo-static approach. Considering the characteristic failure mechanisms of layered slopes under seismic loading, a lattice-type anchor-rod reinforcement system is proposed. The influence of this system on the stress field, displacement field, and safety factor is investigated under both natural and seismic conditions. The results indicate that the lattice anchor-rod system markedly enhances slope stability, significantly increasing the safety factor in both loading scenarios. Under seismic excitation, the layered slope develops an extensive failure slip surface, with the maximum displacement concentrated at the slope toe.

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