Physical modeling is an effective method for studying the failure process of locked-segment
type landslides, whose stability is governed by the locking section along the potential slip …

During or immediately after rainfall many slope failures have been observed. The slope
failure occurred due to rainfall infiltration that rapidly increase the pore pressure and trigger …

The characteristics of debris flows (eg, mobility, sediment concentration, erosion, and
deposition of sediment) are dependent on the pore water pressure in the flows. Therefore …

The paper investigates the initiation mechanism of debris flow through the survey with
detailed analysis for several field debris flow events. The field investigation shows that the …

Soil mass failure disasters are among the most destructive disasters in mountainous areas
worldwide, and they continue to receive significant attention in the literature. However …

Early warning model of debris flow is important for providing local residents with reliable and
accurate warning information to escape from debris flow hazards. This research studied the …

Debris flows are powerful, geophysical flows with the potential to cause fatalities and
damage infrastructure. The hazard posed by these events is often related to the velocity of …

The design of debris flow protective structures has represented a challenge since the last
decades. The design process might consider several variables related to actions and …

The characteristics of debris flows (eg, mobility, sediment concentration, erosion, and
deposition of sediment) are dependent on the pore-water pressure in the flows. Therefore …

Bouldery debris flows exhibit a rich variety of dynamics including complex fluid-like
behaviour and spontaneous pattern formation. A predictive model for these flows is elusive …