Dynamic characteristics determine the mobility of debris flow and are also key to hazard risk assessment. However, the dynamic process of natural debris flow is very complex. Based on the systematic analysis of the field observation data of 93 debris-flow events at Jiangjia Ravine (Yunnan, China), this study attempts to investigate the dynamic mechanisms and sources of flow resistance of debris flow. The Jiangjia Ravine debris flows are almost completely liquefied, indicating that grain contact friction plays a negligible role. Flow regime analysis shows that the flow regimes of the Jiangjia Ravine debris flows varie from viscous to inertial. The fluid viscous effect and particle collisions may be the main sources of flow resistance
Debris flow is one of the major secondary mountain hazards following the earthquake. This study expl...
Debris flow hazard posts a big threat to the main downstream of Jinsha River where a number of huge ...
Various types of flow or mass movement involving water and sediments occur on steep slopes in mounta...
Dynamic characteristics determine the mobility of debris flow and are also key to hazard risk assess...
The 2008 Wenchuan earthquake induced a large number of landslides, and a vast amount of loose landsl...
Non-homogeneous debris flows generally occur during the rainy seasons in Southwest China, and have r...
Non-homogeneous debris flows generally occur during the rainy seasons in Southwest China, and have r...
The 2008 Wenchuan earthquake triggered an exceptional number of landslides. The large amount of loos...
The principal objectives of this research are to investigate the flow mechanisms of debris flows. Th...
Non-homogeneous debris flows are characterized by a wide grain size gradation, high volumetric weigh...
Non-homogeneous debris flows are characterized by a wide grain size gradation, high volumetric weigh...
Debris flow is a devastating natural hazard phenomenon in mountainous areas, which causes human loss...
Debris flow is generally composed of a wide range of solid particles and viscous pore fluid. It flow...
Abstract: As one of dominate geological disaster and geomorphologic processes in mountains, debris f...
On 28 June 2012, a large debris flow occurred in Aizi gully, Ningnan County, Sichuan Province, China...
Debris flow is one of the major secondary mountain hazards following the earthquake. This study expl...
Debris flow hazard posts a big threat to the main downstream of Jinsha River where a number of huge ...
Various types of flow or mass movement involving water and sediments occur on steep slopes in mounta...
Dynamic characteristics determine the mobility of debris flow and are also key to hazard risk assess...
The 2008 Wenchuan earthquake induced a large number of landslides, and a vast amount of loose landsl...
Non-homogeneous debris flows generally occur during the rainy seasons in Southwest China, and have r...
Non-homogeneous debris flows generally occur during the rainy seasons in Southwest China, and have r...
The 2008 Wenchuan earthquake triggered an exceptional number of landslides. The large amount of loos...
The principal objectives of this research are to investigate the flow mechanisms of debris flows. Th...
Non-homogeneous debris flows are characterized by a wide grain size gradation, high volumetric weigh...
Non-homogeneous debris flows are characterized by a wide grain size gradation, high volumetric weigh...
Debris flow is a devastating natural hazard phenomenon in mountainous areas, which causes human loss...
Debris flow is generally composed of a wide range of solid particles and viscous pore fluid. It flow...
Abstract: As one of dominate geological disaster and geomorphologic processes in mountains, debris f...
On 28 June 2012, a large debris flow occurred in Aizi gully, Ningnan County, Sichuan Province, China...
Debris flow is one of the major secondary mountain hazards following the earthquake. This study expl...
Debris flow hazard posts a big threat to the main downstream of Jinsha River where a number of huge ...
Various types of flow or mass movement involving water and sediments occur on steep slopes in mounta...