.png){kind=icon}
.png){kind=icon}
Return
Linking debris flow erosion to channel-bed parameters: Geotechnical and UAS-based investigation of ten channels in Switzerland
.png){kind=icon}
OA
AI
H
F
P
A
A
Y
J
B
F
C
R
P
J
DOI：10.1016/j.geomorph.2026.110360.png)
.png){kind=icon}
.png){kind=icon}
Share.png){kind=icon}
Save
Abstract
En 中文
• UAS surveys show erosion dominates on steep slopes but varies between channels. • We collect a multi-site dataset of geotechnical properties of channel-bed sediments. • Fine-grained beds with low permeability show higher average erosion. • Wet fresh debris flow deposits are weaker than bed material left after erosion. • Four channel types emerge: small–coarse, intermediate–coarse/fine, large–fine.
Keywords:
Debris flows
Landslides
Erosion
Deposition
Unmanned aerial system
Field investigations
Permeability
AI Summary
Key information extracted from the uploaded paper, including a brief overview, abstract, background, key highlights, visual analysis, and future outlook.
Journal
IF:
3.3
Papers:
8.5K
Citations:
2.8W
Organization
Cited Papers