Avalanche mobility induced by the presence of an erodible bed and associated entrainment
By Anne Mangeney, Lev S. Tsimring, D. Volfson, Igor S. Aranson, François Bouchut. 2007
137 citations recorded by the source corpus.
Subfields: Computational Mechanics, Management, Monitoring, Policy and Law, Ocean Engineering
View Paper: https://www.semanticscholar.org/paper/9db528f8245726f9798a02f2f2a293ada3b2258e
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Computational Mechanics
In Management, Monitoring, Policy and Law
In Ocean Engineering
Citations in the corpus
- Fundamental changes of granular flow dynamics, deposition, and erosion processes at high slope angles: Insights from laboratory experiments (2014, methodology): “D topographies [e.g., Denlinger and Iverson , 2001; Bouchut et al. , 2003; Bouchut and Westdickenberg , 2004; Denlinger and Iverson , 2004; Mangeney et al. , 2007b].”
- Numerical modeling of 2‐D granular step collapse on erodible and nonerodible surface (2009, background): “This causes the entrainment of this material and the change in behavior and mobility of the flowing material [Hungr and Evans, 2004; Mangeney et al., 2007; Crosta et al., 2007b, 2009].”
- Insights into rock-ice avalanche dynamics by combined analysis of seismic recordings and a numerical avalanche model (2010, background): “In certain cases, the presence of an erodible ground layer can strongly increase the mobility of granular material [Mangeney et al., 2007], while in other cases the runout distance might be reduced due to momentum transfer from the moving mass to the static underlying erodible ground [McDougall and ”