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黄土沟壑区小型滑坡致大灾及其机理

Small Landslide and Disaster-Causing Mechanism in Gully Loess Area

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【作者】 范立民李勇宁奎斌滕宏泉王启耀张新宇

【Author】 Fan Limin;Li Yong;Ning Kuibin;Teng Hongquan;Wang Qiyao;Zhang Xinyu;Shananxi Institute of Geo-Environment Monitoring;Department of Land and Resources of Shaanxi Province;Key Laboratory of Western China’s Mineral Resources and Geological Engineering,Ministry of Education,Chang’an University;

【机构】 陕西省地质环境监测总站陕西省国土资源厅长安大学西部矿产资源与地质工程教育部重点实验室

【摘要】 发生于延安市甘泉县马岔沟的黄延高速公路14标段的滑坡灾害,滑坡体小但灾情严重,造成19人死亡、2人受伤。滑坡体滑向285°,滑动块体长约12 m,宽约10 m、厚约3 m,体积约360 m3,为一小型黄土滑坡。调查发现,滑坡体位于黄土沟壑区,属于地质灾害高易发区,后缘有一长大裂缝,为古滑坡体的一部分。形成原因主要是高陡边坡的存在,加之滑坡体上部储水设施引水管漏水,长期浸润,导致滑坡体含水量高达31%以上,最终形成一个规模小、滑距长、速度快的飞跃式滑坡,滑坡体直接砸在坡脚下的工棚上,致灾严重。提出了加强黄土沟壑区工棚、建筑工地选址论证和地质灾害监测的建议。

【Abstract】 At 21: 10 on October 10,2014,a landslide hazard occurred to the 14 th section of the Huangyan Express Way located at Machagou,Ganquan County,Yanan City. It caused 19 deaths and 2 injuries. The slip mass in 12 m long,10 m wide,3m thick with a volume about 360 m3 sliding 270°. It is a small landslide of loess.According to the investigation,the slip mass is located in the gully loess area which is an easy occurrence area of geological disaster. There is a large and long gap at the back edge which a part of the ancient slip mass. It is formed mainly for the existence of the high and steep slopes. Besides,the long term infiltration of pipe leakage of water storage facilities at the upper side of the slip mass causes the water content as high as over 31%,thus finally causes the formation of a leap type landslide of small scale,long distance and rapid speed. The slip mass directly hit on the word sheds at the foot of the slope and cause serious disasters. Arguments on strengthening work sheds and selection of constructions as well as suggestions on geological disaster monitoring are proposed.

【基金】 国家重点基础研究发展计划“973”项目“黄土重大灾害及灾害链的发生、演化机制与防控理论”(2014CB744700)
  • 【文献出处】 灾害学 ,Journal of Catastrophology , 编辑部邮箱 ,2015年03期
  • 【分类号】P642.22
  • 【被引频次】40
  • 【下载频次】2626
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