摘要
The Boddhidharma trench in Mentougou District of Beijing City is an ancient debris blow trench, where have occurred several times severe debris flow disasters. The conditions of geology, landform, hydro-meteorology, soil cover and human beings engineering activities are analyzed by using field investigation, geological exploration and laboratory experiment. The properties of debris flow is ascertained to be turbulent or transitional valley-shape debris flow with high density and low viscosity induced by heavy rainfall. The material conditions are primarily studied by the means of particle analysis, electron microscope scanning, X-ray diffraction analysis and laboratory experiment. Finally, the comprehensive countermeasures are put forward.