土工基础 ›› 2026, Vol. 40 ›› Issue (1): 72-74.

• 专题论述 • 上一篇    下一篇

公路边坡泥岩层水力耦合环境下流变破坏机理分析

邢文博   

  1. (中建材广西勘测规划设计有限公司,广西桂林 541002)
  • 收稿日期:2024-01-22 修回日期:2024-01-26 出版日期:2026-02-28 发布日期:2026-04-22
  • 作者简介:邢文博(1993-),男,工程师,研究方向为岩土工程。

Analysis of Rheological Failure Mechanism of Highway Mudstone Slope under Hydraulic Coupling Environment

XING Wenbo   

  1. (CNBM Guangxi Institute of Survey Planning and Design Co. Ltd., Guilin 541002)
  • Received:2024-01-22 Revised:2024-01-26 Online:2026-02-28 Published:2026-04-22

摘要: 泥岩作为边坡的下伏岩层,受水环境及开挖卸荷而改变边界条件的影响,常引发上部岩体的失稳破坏。以广西某既有市政公路边坡治理工程为对象,采用工程地质调查、室内岩石试验及坡体变形监测等方法,综合分析该公路边坡在水力耦合环境下的破坏机理。研究表明:边坡泥岩岩层受积水浸泡饱和,以及边界约束解除和上部载荷变化情况下,发生明显的蠕变变形,变形的累积达到破坏阈值,导致岩层沉降,最终引起上部岩层沉陷而张拉或剪切破坏。基于该破坏机理,针对性地对该边坡进行了有效的治理,对相似工程具有类比和参考的意义。

关键词: 泥岩, 水力耦合作用, 流变

Abstract: Mudstone, as the underlying bedrock layer of a slope, is often affected by changes in boundary conditions caused by water environment and excavation unloading, which often leads to instability and failure of the upper rock mass. An existing municipal highway slope treatment project in Guangxi is presented in this paper as the case history. Evaluation methods such as engineering geological investigation, laboratory rock testing, and slope deformation monitoring are performed to comprehensively analyze the failure mechanism of the highway slope in a hydraulic coupling environment. Research has shown that the mudstone rock layer on the slope undergoes significant creep deformation due to the saturation caused by waterlogging, as well as the release of boundary constraints and changes in upper loads. The accumulation of deformation reaches the failure threshold, leading to rock subsidence and ultimately causing tensile or shear failure of the upper rock layer. Based on this failure mechanism, the effective treatment was carried out on the slope in a controlled manner, thereby validating the mechanism analysis in this study, and having analogical and reference significance for similar projects.

Key words: Mudstone, Hydraulic Coupling Effect, Rheology

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