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静宁县田堡调蓄水池滑坡成因及稳定性分析

韩朝君 李国营 吴玮江 张立军 韩海龙

中国地质灾害与防治学报2023,Vol.34Issue(6):13-19,7.
中国地质灾害与防治学报2023,Vol.34Issue(6):13-19,7.DOI:10.16031/j.cnki.issn.1003-8035.202305036

静宁县田堡调蓄水池滑坡成因及稳定性分析

Causes and stability analysis of the landslide at Tianbao Reservoir in Jingning County,Gansu Province

韩朝君 1李国营 1吴玮江 2张立军 1韩海龙1

作者信息

  • 1. 甘肃省地质矿产勘查开发局第二地质矿产勘查院,甘肃兰州 730020
  • 2. 甘肃省科学院地质自然灾害防治研究所,甘肃兰州 730000
  • 折叠

摘要

Abstract

On September 18,2020,a landslide occurred on the left bank of Tianbao Reservoir in Tianbao Village,Sihe Town,Jingning County,Pingliang City,Gansu Province.The landslide is 180 m long,240 m wide,48.5×104 m3 in volume,and 191° in main sliding direction,which is the revival of the old loess-mudstone landslide.Landslide destroys the excavated slope and highway subgrade,which seriously threatens the normal construction of Tianbao Reservoir.Through field investigation,geotechnical test and calculation,the geological conditions,basic characteristics and causes of landslide formation in Tianbao Reservoir were discussed,and the stability of landslide was analyzed by simplified Janbu method.The study found that the formation conditions of the landslide are mainly three aspects:the geological foundation of the old landslide,the excavation of the front edge of the slope,and the continuous heavy rainfall.That is,the old landslide is caused by the large-scale excavation of the slope toe and the heavy rainfall.The stability calculation results show that after excavating the slope toe,the stability coefficient is less than 0.98 under the rainstorm condition,which is in the unstable sliding state.After sliding,the stability coefficient of each working condition is less than 1.05,which is in the unstable-unstable state.

关键词

滑坡/成因/工程开挖/降水/稳定性

Key words

landslide/genesis/engineering excavation/precipitation/stability

分类

天文与地球科学

引用本文复制引用

韩朝君,李国营,吴玮江,张立军,韩海龙..静宁县田堡调蓄水池滑坡成因及稳定性分析[J].中国地质灾害与防治学报,2023,34(6):13-19,7.

基金项目

甘肃省科学院应用研究与开发项目(2022JK-04) (2022JK-04)

中国地质灾害与防治学报

OACSCDCSTPCD

1003-8035

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