CAJ | 학술논문

2012年5月31日黄莲树滑坡前缘发生大规模滑动,顺坡向下滑动约8~9 m,因监测预警及时,幸未发生人员伤亡。本文通过对黄莲树滑坡历年来监测资料的分析,得出滑坡变形特征及其变形启动机理,并总结出了以库水位升降和大气降雨为主的滑坡稳定性影响因素,通过 ABAQUS数值模拟软件计算验证了这一结论。
2012년5월31일황련수활파전연발생대규모활동,순파향하활동약8~9 m,인감측예경급시,행미발생인원상망。본문통과대황련수활파력년래감측자료적분석,득출활파변형특정급기변형계동궤리,병총결출료이고수위승강화대기강우위주적활파은정성영향인소,통과 ABAQUS수치모의연건계산험증료저일결론。
In May 31,2012,the front of Huanglianshu landslide slid down about 8-9 m along the slope.For-tunately,there were no casualties due to its monitoring and early warning timely.Through analysing monito-ring deformation data of Huanglianshu landslide over the years,the authors arrive at the landslide deforma-tion characteristics and starting mechanism,and summarize the factors affecting the stability of landslide un-der reservoir water level fluctuation and the atmospheric rainfall,and then through the numerical simulation software ABAQUS to verify the conclusion as well.