Debris flows are among the most catastrophic natural phenomena, attracting the interest of
researchers, engineers and government agencies. The complexity of the physical process …

This paper presents a model which can be used for fast landslides where coupling between
solid and pore fluid plays a fundamental role. The proposed model is able to describe debris …

A debris flow is one of the most dangerous types of geophysical mass flows moving
downward mountain slopes and consist of a mixture of soil and rocks with a significant …

Debris flows are a type of fast landslides where a mixture of soil and water propagates along
narrow channels. The main characteristics are (1) important relative displacements between …

Affected by continuous heavy rainfall, a large number of landslide disasters occur every year
in the Three Gorges Reservoir area, which causes serious property loss and casualties. In …

In mountainous-forested landscape, quantifying the materials produced at hillslope scale
that effectively reach the channel network with a given probability is currently challenging …

Societal risks associated with debris flow hazards are significant and likely to escalate due
to global population growth trends and the compounding effects of climate change …

Debris flows are dangerous phenomena due to their large run-out distances and high
velocities. The time-space evolution of the interstitial pore water pressures much affects the …

Slow and very slow landslides can cause severe economic damage to structures. Due to
their velocity of propagation, it is possible to take action such as programmed maintenance …

Depth‐averaged thin‐layer models are commonly used to model rapid gravity‐driven flows
such as debris flows or debris avalanches. However, the formal derivation of thin‐layer …