This paper is devoted to analyze the micro-mechanical behavior of snow layers subjected to shear force. A number of cold laboratory tests were performed on reconstructed snow samples on a specially designed direct shear apparatus and the loading process leading to the failure was recorded by a high-speed camera. The specimens were prepared under isothermal conditions and immediately tested in order to avoid sintering between the snow grains. Image analysis techniques (digital image correlation and particle image velocimetry) were applied on the camera records in order to obtain the snow strain history (during the loading phase) and the velocity field after the failure. Sequences of jamming and unjamming phases with the formation of vortices...
ABSTRACT: Researchers and practitioners have long utilized a variety of penetrometers to investigat...
ABSTRACT. Dry-snow slab avalanches initiate from a failure in a weak snow layer below a cohesive sla...
International audienceWeak layers of snow are thin layers of low density and cohesion that consist o...
International audienceWeak layers of snow are thin layers of low density and cohesion that consist o...
ABSTRACT: Natural dry-snow slab avalanches start with a failure within a weak snow layer. In order t...
Dry snow slab avalanches release as a result of the failure of a weakly bonded layer located below a...
Weak layers of snow are thin layers of low density and cohesion that consist of a complex network of...
The failure of a weak snow layer underlying a cohesive slab is the primary step in the release proce...
Dry-snow slab avalanches start with the formation of a local failure in a highly porous weak layer u...
Dry-snow slab avalanches start with a failure in a weak snow layer below a cohesive snow slab of amp...
[Departement_IRSTEA]Eaux [ADD1_IRSTEA]Hydrosystèmes et risques naturelsInternational audienceThe mec...
International audienceThe mechanical behavior of snow weak layers is a crucial element in dry snow s...
Snowpack weak layers may fail due to excess stresses of various natures, caused by snowfall, skiers,...
Understanding failure initiation within weak snow layers is essential for modeling and predicting dr...
ABSTRACT: Researchers and practitioners have long utilized a variety of penetrometers to investigat...
ABSTRACT. Dry-snow slab avalanches initiate from a failure in a weak snow layer below a cohesive sla...
International audienceWeak layers of snow are thin layers of low density and cohesion that consist o...
International audienceWeak layers of snow are thin layers of low density and cohesion that consist o...
ABSTRACT: Natural dry-snow slab avalanches start with a failure within a weak snow layer. In order t...
Dry snow slab avalanches release as a result of the failure of a weakly bonded layer located below a...
Weak layers of snow are thin layers of low density and cohesion that consist of a complex network of...
The failure of a weak snow layer underlying a cohesive slab is the primary step in the release proce...
Dry-snow slab avalanches start with the formation of a local failure in a highly porous weak layer u...
Dry-snow slab avalanches start with a failure in a weak snow layer below a cohesive snow slab of amp...
[Departement_IRSTEA]Eaux [ADD1_IRSTEA]Hydrosystèmes et risques naturelsInternational audienceThe mec...
International audienceThe mechanical behavior of snow weak layers is a crucial element in dry snow s...
Snowpack weak layers may fail due to excess stresses of various natures, caused by snowfall, skiers,...
Understanding failure initiation within weak snow layers is essential for modeling and predicting dr...
ABSTRACT: Researchers and practitioners have long utilized a variety of penetrometers to investigat...
ABSTRACT. Dry-snow slab avalanches initiate from a failure in a weak snow layer below a cohesive sla...
International audienceWeak layers of snow are thin layers of low density and cohesion that consist o...