土工基础 ›› 2025, Vol. 39 ›› Issue (5): 720-724.

• 工程实录 • 上一篇    下一篇

广西某反倾路堑高边坡变形破坏过程分析

邰联欢   

  1. (中交二航局广西建设工程有限公司,南宁 530200)
  • 收稿日期:2023-09-05 修回日期:2023-09-22 出版日期:2025-10-31 发布日期:2025-10-30
  • 作者简介:邰联欢(1991-),男,工程师,研究方向为边坡工程安全与防治等。

Analysis of Deformation and Failure of an Anticline Cutting High Slope in a Guangxi Expressway

TAI Lianhuan   

  1. (CCCC Second Harbor Guangxi Construction Engineering Co. Ltd., Nanning 530200)
  • Received:2023-09-05 Revised:2023-09-22 Online:2025-10-31 Published:2025-10-30

摘要: 针对广西某反倾路堑高边坡在施工过程中的变形破坏模式,通过现场地质调查,并结合变形测试数据,确定了边坡倾倒变形的主要影响因素,在此基础上建立了Phase2有限元分析模型,研究了施工过程中变形形态、滑动面演化和变形发展规律,指出了该边坡的变形破坏演化过程。结果表明:从地质结构来看,反倾岩层层面是倾倒变形破坏的主要影响因素,强风化与中风化的岩层界面决定了滑动面的深度;边坡开挖完成后的安全系数为1.09,滑动面状态为坡脚贯通出露、坡顶完好的欠稳定状态;开挖过程中强、中风化界面发生错动变形、反倾层面倾倒滑移,导致坡面出现台阶状变形形态,随着开挖,逐步向坡脚发展,最终导致边坡出现倾倒变形破坏模式;边坡为倾倒-牵引式破坏模式,其发展演化过程为:开挖扰动岩层界面错动-反倾层面倾倒-下部变形滑动-牵引拉裂上部-倾倒变形破坏。

关键词: 反倾高边坡, 倾倒变形, 破坏模式, 演化过程, 数值模拟

Abstract: The deformation and failure mode of an anticline cutting high slope in Guangxi during the construction process are presented in this paper. The main influencing factors of slope toppling deformation are evaluated through the field geological survey and deformation test data. On this basis, a Phase2 finite element analysis model is established. The deformation morphology, sliding surface evolution and deformation development during the construction process are studied, and the deformation and failure evolution process of the slope are presented. The results show that from the perspective of geological structure, the anticline rock stratum is the main influencing factor of toppling deformation and failure. The interface between the strongly weathered and the moderately weathered rock strata controls the depth of sliding surface. The safety factor of the slope after excavation is 1.09, and the sliding surface is in an unstable state with the slope toe exposed and the slope top intact. In the process of excavation, the strong and medium weathered interface occurs dislocation deformation, and the anticline layer is toppled and slipped, which leads to the stepshaped deformation morphology of the slope surface. With the excavation, it gradually develops to the toe of the slope, which eventually leads to the toppling deformation failure mode of the slope. The slope is a toppling-traction failure mode. Its development and evolution process is excavation disturbance-rock interface dislocation-anticline layer toppling-lower deformation sliding-traction cracking upper-toppling deformation failure.

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