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云南虎跳峡大塘子松散堆积体滑坡形成演化机制分析

Analysis of Forming Evolvement Mechanism of Datangzi Loose Congeries landslide at Tiger-Leaping Gorge in Yunnan Province

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【作者】 刘衡秋胡瑞林周宏磊朱志刚

【Author】 Liu Hengqiu1 Hu Ruilin2 Zhou Honglei1 Zhu Zhigang1(1.BGI Engineering Consultants Ltd.,Beijing 100038,China;2.Key Laboratory of Engineering Geomechanics,Chinese Academy of Sciences,Beijing 100029,China)

【机构】 北京市勘察设计研究院有限公司中国科学院工程地质力学重点实验室

【摘要】 大塘子滑坡属于我国西南地区典型的第四纪崩坡积松散堆积体滑坡.从滑坡的发育特征调查和资料收集入手,研究了该滑坡的形成条件和演化机制,分析认为降雨和地震联合作用诱发滑坡的产生,且滑坡具有明显的周期性,其形成过程经历"碎石体堆积-自然休止状态-显著滑动"3个演化阶段,存在再次滑动的可能性,其周期长短主要受降雨强度和地震活动的影响.这一结果对于合理部署区域防灾减灾具有指导意义.

【Abstract】 Datangzi landslide is a typical Quaternary period loose congeries landslide in Southwest China.The detailed studies of the forming condition and evolvement mechanism of Datangzi landslide were carried out based on in-situ surveys and data collection.It is shown that the combination of prolonged rainfall and the Lijiang earthquake should be the main cause of the landslide;and the landslide may revive in some day.One development process includes three main phases such as avalanche accumulation,nature inactivity and gliding;and its cycle length is mainly affected by rainfall intensity and the impact of seismic activities.This study will provide a practical example for alleviating and preventing geo-hazards in Southwest China.

【基金】 国家科技部“十一五”科技支撑项目(2006BAJ06B02);国家重点基础研究(973)项目(2002CB412702)
  • 【文献出处】 三峡大学学报(自然科学版) ,Journal of China Three Gorges University(Natural Sciences) , 编辑部邮箱 ,2010年02期
  • 【分类号】P642.22
  • 【被引频次】5
  • 【下载频次】200
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