Author
Listed:
- Andrin Caviezel
(WSL Institute for Snow and Avalanche Research SLF)
- Adrian Ringenbach
(WSL Institute for Snow and Avalanche Research SLF)
- Sophia E. Demmel
(WSL Institute for Snow and Avalanche Research SLF)
- Claire E. Dinneen
(WSL Institute for Snow and Avalanche Research SLF)
- Nora Krebs
(WSL Institute for Snow and Avalanche Research SLF)
- Yves Bühler
(WSL Institute for Snow and Avalanche Research SLF)
- Marc Christen
(WSL Institute for Snow and Avalanche Research SLF)
- Guillaume Meyrat
(WSL Institute for Snow and Avalanche Research SLF)
- Andreas Stoffel
(WSL Institute for Snow and Avalanche Research SLF)
- Elisabeth Hafner
(WSL Institute for Snow and Avalanche Research SLF)
- Lucie A. Eberhard
(WSL Institute for Snow and Avalanche Research SLF)
- Daniel von Rickenbach
(WSL Institute for Snow and Avalanche Research SLF)
- Kevin Simmler
(WSL Institute for Snow and Avalanche Research SLF)
- Philipp Mayer
(ETH Zurich, Integrated Systems Lab IIS)
- Pascal S. Niklaus
(ETH Zurich, Integrated Systems Lab IIS)
- Thomas Birchler
(ETH Zurich, Integrated Systems Lab IIS)
- Tim Aebi
(ETH Zurich, Integrated Systems Lab IIS)
- Lukas Cavigelli
(ETH Zurich, Integrated Systems Lab IIS)
- Michael Schaffner
(ETH Zurich, Integrated Systems Lab IIS)
- Stefan Rickli
(ETH Zurich, Integrated Systems Lab IIS)
- Christoph Schnetzler
(ETH Zurich, Integrated Systems Lab IIS)
- Michele Magno
(ETH Zurich, Integrated Systems Lab IIS)
- Luca Benini
(ETH Zurich, Integrated Systems Lab IIS)
- Perry Bartelt
(WSL Institute for Snow and Avalanche Research SLF)
Abstract
The mitigation of rapid mass movements involves a subtle interplay between field surveys, numerical modelling, and experience. Hazard engineers rely on a combination of best practices and, if available, historical facts as a vital prerequisite in establishing reproducible and accurate hazard zoning. Full-scale field tests have been performed to reinforce the physical understanding of debris flows and snow avalanches. Rockfall dynamics are - especially the quantification of energy dissipation during the complex rock-ground interaction - largely unknown. The awareness of rock shape dependence is growing, but presently, there exists little experimental basis on how rockfall hazard scales with rock mass, size, and shape. Here, we present a unique data set of induced single-block rockfall events comprising data from equant and wheel-shaped blocks with masses up to 2670 kg, quantifying the influence of rock shape and mass on lateral spreading and longitudinal runout and hence challenging common practices in rockfall hazard assessment.
Suggested Citation
Andrin Caviezel & Adrian Ringenbach & Sophia E. Demmel & Claire E. Dinneen & Nora Krebs & Yves Bühler & Marc Christen & Guillaume Meyrat & Andreas Stoffel & Elisabeth Hafner & Lucie A. Eberhard & Dani, 2021.
"The relevance of rock shape over mass—implications for rockfall hazard assessments,"
Nature Communications, Nature, vol. 12(1), pages 1-9, December.
Handle:
RePEc:nat:natcom:v:12:y:2021:i:1:d:10.1038_s41467-021-25794-y
DOI: 10.1038/s41467-021-25794-y
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