The physics of debris flows¶
Iverson. The physics of debris flows. Reviews of Geophysics.
Cited by¶
1 citation across 1 artifact.
Each citation links to the sentence it supports in the citing article.
Domain-specific¶
- Mass Wasting
- Landslides, slumps, and rotational failures — the classic slope-failure events with identifiable shear surfaces, the home case for factor-of-safety analysis. Rockfalls and topples — discrete-block detachment from cliff faces under freeze-thaw, root wedging, or undercutting. Debris flows and lahars — water-saturated mass movement common after wildfire (Santa Barbara) or eruption (Nevado del Ruiz), where pore pressure and rheology govern long, fast runout
This sourceReviews of Geophysics, 1997. That high pore-fluid pressures and the resulting debris-flow rheology strongly mediate grain interactions and enhance debris-flow mobility.
Supported in partVerified against the publisher's abstract
“In debris flows, however, pore fluid that is highly viscous and nearly incompressible, composed of water with suspended silt and clay, can strongly mediate intergranular friction and collisions.”
- Landslides, slumps, and rotational failures — the classic slope-failure events with identifiable shear surfaces, the home case for factor-of-safety analysis. Rockfalls and topples — discrete-block detachment from cliff faces under freeze-thaw, root wedging, or undercutting. Debris flows and lahars — water-saturated mass movement common after wildfire (Santa Barbara) or eruption (Nevado del Ruiz), where pore pressure and rheology govern long, fast runout
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