Results 1 to 10 of about 2,160 (115)
Fracture toughness of mixed-mode anticracks in highly porous materials [PDF]
When porous materials are subjected to compressive loads, localized failure chains, commonly termed anticracks, can occur and cause large-scale structural failure.
Valentin Adam +4 more
doaj +3 more sources
Role of Ice Mechanics on Snow Viscoplasticity
The porous structure of snow becomes denser with time under gravity, primarily due to the creep of its ice matrix with viscoplasticity. Despite investigation of this behavior at the macroscopic scale, the driving microscopic mechanisms are still not well
Louis Védrine +4 more
doaj +2 more sources
Crack propagation speeds in weak snowpack layers
For the release of a slab avalanche, crack propagation within a weak snowpack layer below a cohesive snow slab is required. As crack speed measurements can give insight into underlying processes, we analysed three crack propagation events that occurred ...
Bastian Bergfeld +9 more
doaj +1 more source
Temporal evolution of crack propagation characteristics in a weak snowpack layer: conditions of crack arrest and sustained propagation [PDF]
For a slab avalanche to release, we need sustained crack propagation in a weak snow layer beneath a cohesive snow slab – a process we call dynamic crack propagation. Field measurements on crack propagation are very scarce. We therefore performed a series
B. Bergfeld +8 more
doaj +1 more source
Modeling spatially distributed snow instability at a regional scale using Alpine3D
Assessing the avalanche danger level requires snow stratigraphy and instability data. As such data are usually sparse, we investigated whether distributed snow cover modeling can be used to provide information on spatial instability patterns relevant for
Bettina Richter +3 more
doaj +1 more source
Automated prediction of wet-snow avalanche activity in the Swiss Alps
Wet-snow avalanches are triggered by the infiltration of liquid water which weakens the snowpack. Wet-snow avalanches are among the most destructive avalanches, yet their release mechanism is not sufficiently understood for a process-based prediction ...
Martin Hendrick +6 more
doaj +1 more source
Disentangling creep and isothermal metamorphism during snow settlement with X-ray tomography
Once fallen, snow settles due to the combined effects of metamorphism and deformation of the ice matrix under gravity. To understand how these coupled processes affect snow evolution, we performed oedometric compression tests and continuously monitored ...
Antoine Bernard +3 more
doaj +1 more source
Sliding friction on ice and snow is characteristically low at temperatures common on Earth’s surface. This slipperiness underlies efficient sleds, winter sports, and the need for specialized tires. Friction can also play a micro-mechanical role affecting
James H. Lever +3 more
doaj +1 more source
From field observations, dry snow slab avalanche initiation is associated with fracture within relatively thin weak layers under stronger, cohesive slabs.
D. M. McCLUNG, C. P. BORSTAD
doaj +1 more source
Angle of repose experiments with snow: role of grain shape and cohesion
Snow appears as a granular material in most engineering applications. We examined the role of grain shape and cohesion in angle of repose experiments, which are a common means for the characterization of granular materials. The role of shape was examined
Carolin Willibald +4 more
doaj +1 more source

