摘要
首次提出了滑坡岩体高速碰撞模型实验方法。通过实验,研究了滑体碰撞解体后不同速度段岩体体积的分布规律,得出了加速块体所占比例基本与滑体体积及碰撞速度无关,而个别块体获得的加速效应与滑坡体积及碰撞速度有明显的正相关关系。
The method of collisionexperiment of highspeed rockslide was presented. With the experiment, the volume distribution of rock masses with varied speeds after collision was investigated. Experiment results show that the volume of the landslide and its collisionspeed have almost no effect on the volume ratio of speedup rock masses, the maximum speed of the masses has a positive correlation with the volume and collision speed.
出处
《水文地质工程地质》
CAS
CSCD
2003年第6期85-88,共4页
Hydrogeology & Engineering Geology
