摘要
黄土高原是我国地质灾害最为发育的地区之一,其中降雨诱发的浅层黄土滑坡又最为典型。以典型黄土地貌区-柳林县为例,应用SINMAP模型,探讨模型在黄土地区的适用性,分析了随着研究区内降雨量的增加,滑坡变形失稳区域的面积变化、分布位置和扩展趋势。研究表明,随着降雨量的增加,滑坡所处位置逐渐由稳定状态向失稳状态发展,位于失稳分区的滑坡数量逐渐增加,说明降雨对该研究区的斜坡稳定性影响较为明显。通过将模拟结果与实际发生的由降雨触发的滑坡灾害进行对比分析,可以得出SINMAP模型在黄土地区,对区域性降雨诱发浅层黄土滑坡稳定性的模拟预测有效,可以用于黄土地区浅层滑坡的稳定性评价研究。
Loess Plateau is one of the most developed areas of geological disasters in China,and the shallow loess landslide induced by rainfall is the most typical.Taking Liulin County,a typical loess landform area,as an example.With the increase of rainfall in the study area,the area change,distribution location and expansion trend of the landslide deformation instability area are analyzed.The research shows that with the increase of rainfall,the location of landslides gradually develops from a stable state to an unstable state,and the number of landslides in the unstable zone gradually increases,indicating that rainfall has a significant impact on the slope stability of the study area.By comparing the simulation results with the actual rainfall-triggered landslide disasters.It can be concluded that the SINMAP model is effective in simulating and predicting the regional stability of shallow loess landslide induced by rainfall in the loess region,as well as can be used in the stability assessment of shallow landslide in the loess region.
作者
李艳杰
唐亚明
邓亚虹
宋焱勋
慕焕东
山聪
崔思颖
LI Yanjie;TANG Yaming;DENG Yahong;SONG Yanxun;MU Huandong;SHAN Cong;CUI Siying(College of Geology Engineering and Geomatics,Chang’an University,Xi’an,Shaanxi 710054,China;Xi’an Center of China Geological Survey,Xi’an,Shaanxi 710054,China;Institute of Geotechnical Engineering,Xi’an University of Technology,Xi’an,Shaanxi 710048,China)
出处
《中国地质灾害与防治学报》
CSCD
2022年第2期105-114,共10页
The Chinese Journal of Geological Hazard and Control
基金
国家自然科学基金项目(41772275)
中国地质调查局地质调查项目(DD20190642)
陕西省教育厅科学研究计划专项项目(20JK0801)
陕西省自然科学基础研究计划一般项目(2022JQ-289)。
