土工基础 ›› 2022, Vol. 36 ›› Issue (3): 375-378.

• 工程实录 • 上一篇    下一篇

湖北某公路滑坡滑动机理研究

雷奇果1,程 微2   

  1. (1.中交第二公路勘察设计研究院有限公司,武汉 430052;2.中建二局第三建筑工程有限公司,北京 100071)
  • 收稿日期:2022-03-31 修回日期:2022-04-20 出版日期:2022-06-30 发布日期:2022-06-24
  • 作者简介:雷奇果(1989-),男,工程师,研究方向为道路勘察、岩土工程勘察设计。

Factors Contributing to a Highway Landslide in Hubei

LEI Qiguo1, CHENG Wei2   

  1. (1.CCCC Second Highway Survey, Design Institute Co. Ltd., Wuhan 430052;
    2.Third Construction Engineering Co., Ltd., China Construction Second Engineering Bureau, Beijing 100071)
  • Received:2022-03-31 Revised:2022-04-20 Online:2022-06-30 Published:2022-06-24

摘要: 湖北某高速公路在路堤施工完毕后,在持续暴雨条件下,出现路面持续性轻微开裂,路基坡脚挡墙发生局部位移及开裂。该段路基长约160 m,左侧为边坡,右侧为路堤及挡土墙,填土最大高度为8 m,挡墙底部岩溶槽谷极发育,覆盖层最大厚度达8 m,下伏基岩为灰岩夹薄层页岩,岩层褶曲,路基右侧边坡岩层倾向与坡向相反,属逆向坡;左侧路堤岩层倾向与坡向小角度斜角,倾角较缓,属顺向坡;病害给路堤变更设计及施工带来很大的困难。通过分析路基所处的地质构造、地层岩性、水文地质条件、填土特征以及变形监测成果,综合判定该病害为推移式滑坡,处于欠稳定状态。

关键词: 滑坡, 地质条件, 成因, 软弱夹层, 推移式

Abstract: Tensional cracks were observed at the top, toe of slopes as well as the retaining walls of a newly constructed highway embankment in Hubei Province after a prolonged heavy precipitation. The length of this embankment is approximately 160 meters with a slope one the left-hand side and retaining wall at the right-hand side. The maximum backfill height of the embankment is 8 meters. The maximum overburden soil thickness is 8 meters on the well-developed karstic rock pinnacles. The limestone with thin layers of shale bedrock is severely folded with bedding planes that is anticline to the direction of slope at right hand side. The day-lighted bedrock bedding plane has a small angle to the direction of the embankment slope at left hand side. The observed geohazards induced significant difficulties so that many change of design and construction occurred. Based on the geological conditions, soil and rock stratigraphy, hydrological conditions, embankment backfill characteristics and deformation monitoring results, it is concluded that the defects observed is a translational movement and the target embankment is at the instable condition. 

Key words: landslide, geological conditions, contribution factors, weak layer, translational movement

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