摘要
灾害区域地质构造活动强烈,山体破碎,坡度陡峭,岩石风化严重,一旦在地震、暴雨及融雪等条件下易发生滑坡-碎屑流。本文通过理论计算分析并进行对比,同时运用PFC3D模拟融雪型滑坡—碎屑流在各种工况下的稳定性。
Disaster area develops intensive structure activities. mountain body is broken,slope is steep and rock wheathering is severe in this area,so the landslide and debris flow is easy to happen on the condition of earthquake,heavy rain and melting snow. bytheoretical calculation analysis and comparison,the paper apply PFC^3 Dto simulate different condition stability of the landslide and debris flow at the same time.
出处
《四川建材》
2015年第6期234-236,239,共4页
Sichuan Building Materials
基金
2014年西藏自治区大学生创新性实验训练计划项目(2014XCX013)
