【作者】 王立朝； 胡瑞林； 张作辰； 张鸿儒；

【Author】 Wang lichao~1 Hu ruilin~2 Zhang zuochen~3 Zhang hongru~1 (1.Civil and Construction Engineering College,Beijing Jiaotong University;2.Institute of Geology and Geophysics,Chinese Academy of Sciences;3 Chinese Geology and Environment Investigative Agency)

【机构】 北京交通大学土建学院； 中科院地质与地球物理研究所； 中国地质环境调查局；

【摘要】 由于地质条件较差,黄土坡滑坡区临江崩滑堆积体曾发生多次小规模的滑塌,造成了重大人员伤亡和经济损失.在三峡库区蓄水后,影响库岸稳定的不利因素增加,如果临江崩滑堆积体得不到及时治理,一旦滑塌,后果十分严重,并可能影响到黄土坡滑坡区的整体稳定.为此,根据塌岸的成因,分析了塌岸的形成机制,并有针对性地提出了防治措施。更多还原

【Abstract】 Due to the poor geological conditions of the sediments of Huangtupo landslide areas along the Yangtse River, many small-scale collapses have happened as result of heavy casualties and economic loss.Once the Three Gorges Reservoir areas are sluice,disadvantageous factors influencing on the stability of the bank will increase.If these sediments cannot be controlled without delay,consequences will be disastrous and could also touch the whole stability of the Huangtupo landslide areas.In accordance with the formation of bank collapse,the formative mechanism is analyzed, and some prevention measures are proposed.更多还原