土工基础 ›› 2024, Vol. 38 ›› Issue (2): 299-303.

• 专题论述 • 上一篇    下一篇

贵州某公路长大顺层滑坡成因分析及稳定性评价

雷 青1,刘仕洪,张 亚1,陈 民1,姜 波2   

  1. (1.贵州省铜仁公路管理局,贵州铜仁 554300;2.贵州省交通规划勘察设计研究院股份有限公司,贵阳 550001)
  • 收稿日期:2023-11-01 修回日期:2023-11-16 出版日期:2024-02-29 发布日期:2024-12-22
  • 作者简介:雷青(1978-),男,高级工程师,研究方向为公路建设养护。
  • 基金资助:
    贵州省公路局科技项目(项目编号:2022QLK04);交通运输行业重点科技项目(项目编号:2021-ZD1-021);交通运输行业重点科技项目(项目编号:2022-MS1-058);贵州省交通运输厅科技项目(项目编号:2022-122-003)

Stability Evaluation and Analysis of Landslide in Long Daylighted Bedding of a Highway in Guizhou Province

LEI Qing1, LIU Shihong1, ZHANG Ya1, CHEN Ming1, JIANG Bo2   

  1. (1.Bureau of Guizhou Highway Administration, Tongren 554300;
    2.Guizhou Transportation Planning, Survey and Design Institute Co. Ltd., Guiyang 550001)
  • Received:2023-11-01 Revised:2023-11-16 Online:2024-02-29 Published:2024-12-22

摘要: 为了评价国道G326甘龙滑坡的稳定性,综合现场调查、钻探等手段详细查明了滑坡的工程地质条件及成因,并结合geo-studio软件对考虑强降雨入渗条件下的滑坡进行了稳定性评价。结果表明:滑坡地形相对较陡,下伏基岩顺切,岩土体工程性质较差,雨水长期冲刷形成的长大裂隙切割岩体导致斜坡体临空,构成了长大顺层巨型滑坡形成的基本条件;滑坡前一周降雨强度达到全年最高,坡体后缘浸润线抬升,坡体孔隙水压力陡增,且坡体内部特别是中前部渗透压力达到峰值,斜坡稳定性骤降;强降雨补给引起的渗流作用及孔隙水压力变化是滑坡形成的主要诱发因素。

关键词: 长大顺层滑坡, 成因分析, geostudio, 强降雨, 稳定性评价

Abstract: To evaluate the stability of the Ganlong landslide in National Route G326, the engineering geological conditions and factors that triggering the landslide are identified in detail by the comprehensive field investigation, drilling and other methods. The stability of the landslide under the consideration of the heavy rainfall infiltration is evaluated by the geostudio software. The result shows that the landslide topography is relatively steep, the underlying bedrock is tangential, the engineering properties of rock and soil mass are poor, and the long fissure cutting rock mass formed by the longterm rain erosion leads to the cavitation of the slope body, which constitutes the basic conditions for the formation of a large long daylighted bedding landslide. One week before the landslide, the rainfall intensity reached the highest in the entire year, the infiltration line at the rear edge of the slope raised, the pore water pressure of the slope increased sharply, and the infiltration pressure inside the slope, especially in the middle and front of the slope, reached a peak, and the slope stability sharply reduced. The seepage and pore water pressure induced by the heavy rainfall are the main inducing factors of landslide formation.

Key words: Long Daylighted Bedding Landslide, Cause Analysis, Geostudio, Heavy Rainfall, Stability Evaluation

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