浅层顺层滑坡成灾机制分析及其稳定性评价

朱涛, 翟亚锋, 翟会君. 2023. 浅层顺层滑坡成灾机制分析及其稳定性评价. 中国地质调查, 10(6): 88-94. doi: 10.19388/j.zgdzdc.2023.06.10
引用本文: 朱涛, 翟亚锋, 翟会君. 2023. 浅层顺层滑坡成灾机制分析及其稳定性评价. 中国地质调查, 10(6): 88-94. doi: 10.19388/j.zgdzdc.2023.06.10
ZHU Tao, ZHAI Yafeng, ZHAI Huijun. 2023. Disaster mechanism analysis and stability evaluation of shallow bedding landslide. Geological Survey of China, 10(6): 88-94. doi: 10.19388/j.zgdzdc.2023.06.10
Citation: ZHU Tao, ZHAI Yafeng, ZHAI Huijun. 2023. Disaster mechanism analysis and stability evaluation of shallow bedding landslide. Geological Survey of China, 10(6): 88-94. doi: 10.19388/j.zgdzdc.2023.06.10

浅层顺层滑坡成灾机制分析及其稳定性评价

详细信息
    作者简介: 朱涛(1984—),男,工程师,主要从事地质灾害危险性评估、地质灾害治理施工、山水林田湖草生态修复、地质测绘等领域的工作。Email: zhut1232022@163.com。
  • 中图分类号: P642

Disaster mechanism analysis and stability evaluation of shallow bedding landslide

  • 为准确掌握浅层顺层滑坡的成因机制,合理评价其稳定性,基于滑坡所处地质条件,先开展其成因机制分析,再利用传递系数法和变形预测模型分别开展滑坡稳定性的现状评价及预测评价。实例分析表明: 浅层顺层滑坡的影响因素相对较多,且由于浅层滑坡的滑体厚度较薄,受外界扰动影响易较大,因此,浅层滑坡对各类因素的敏感性均较强。在滑坡稳定性现状评价结果中: 天然工况条件下的稳定性系数为1.21,属稳定状态; 暴雨工况条件下的稳定性系数为1.02,属欠稳定状态; 地震工况条件下的稳定性系数为1.09,属基本稳定状态。在滑坡稳定性预测评价结果中,滑坡各监测点位置处的变形预测速率均一定程度上大于现有变形速率,说明滑坡后续累计变形仍会进一步加速,其说明在本次监测时段后的滑坡稳定性将趋于减弱,需尽快开展此滑坡防治研究。研究成果可为浅层顺层滑坡灾害防治提供一定的理论指导。
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出版历程
收稿日期:  2023-03-14
修回日期:  2023-08-14

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