Pore pressure evolution and entrainment mechanism of convex unsaturated colluvial beds with divergent compositions under debris flow overriding
A debris flow descending through an erodible convex colluvial bed, originating from a landslide dam and its upstream deposits, can entrain massive amounts of sediment, dramatically increasing the debris flow volume. Most existing erosion models assume that bed sediments are fully saturated, although...
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| Principais autores: | , , |
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| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
Elsevier
2026-01-01
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| Serier: | Journal of Rock Mechanics and Geotechnical Engineering |
| Fag: | |
| Online adgang: | http://www.sciencedirect.com/science/article/pii/S1674775525002197 |
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