陕西省南秦岭典型土质滑坡形成机制及风险评价——以商洛市山阳中学滑坡为例
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中国地质调查局地质调查项目“陕西省重要城镇地质灾害调查”(12120113008900);中国地质调查局地质调查项目“秦岭及宁东矿产资源集中开采区地质环境调查”(12120111000150022)


Risk Assessment and Formation Mechanism for Typical Soil Landslide in South Qinling Mountains of Shaanxi Province-Taking Shanyang School Landslide as an Example
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    [目的] 对陕西省南秦岭典型土质滑坡形成机制及风险进行研究和评价,为该区地质灾害的防治提供支持。[方法] 以陕西省商洛市山阳县山阳中学滑坡为研究对象,通过现场调查、勘察及室内试验开展研究。[结果] 山阳中学滑坡现处于基本稳定状态,但不排除遭遇极端气候下复活的可能,滑坡复活概率为7.45%。[结论] 区域地壳差异性运动是山阳中学滑坡形成的内动力因素;降雨是该滑坡启动的主要外在诱因;滑坡威胁范围内人员在最大风险中丧命的年概率为:1.70×10-3

    Abstract:

    [Objective] Studying on the formation mechanism and risk assessment of typical soil landslide in South Qinling Mountains can provide technical support for the prevention of geological disasters in the region.[Methods] The Shanyang School landslide in Shaanxi was selected as an example,the formation conditions and distribution characteristics were analyzed through in situ investigation, survey and laboratory test.[Results] The results show that Shanyang School landslide is in a stable state, the landslide may be revive suffered extreme climates, and resurrection probability is 7.45%.[Conclusion] Regional differences in the crustal movement are the inner dynamic factor of the landslide, and rainfall is the main induced factor of landslide. The maximum personnel risk probability is 1.70×10-3 in the threats range.

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高波,张茂省,贾俊,张成航.陕西省南秦岭典型土质滑坡形成机制及风险评价——以商洛市山阳中学滑坡为例[J].水土保持通报,2016,36(6):97-101,109

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  • 收稿日期:2016-07-04
  • 最后修改日期:2016-10-11
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  • 在线发布日期: 2017-01-13
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