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Indeed, the violent release of gas at depth seems to be a common activity on 67P, followed by the collapse of material back into the void.
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The collapse of granular material submerged in a water is then investigated using a Mixture Model approach.
Uniaxial compressive failure initiates at relatively small strains (≈1 2%) and occurs through a process of crushing and collapse of the material within a localized deformation band.
Finally, by highlighting the basic role played by the loading parameters, the vanishing of the second-order work is shown to be a proper criterion to detect the occurrence of a bifurcation from a quasi-static regime to a dynamic regime leading to the collapse of the material.
Under uniaxial loading, a tensile stress is necessarily balanced in the microstructure by a compressive load on fibers normal to the stretch direction, leading to a collapse of the material in the normal direction and a strong enghancement of fiber alignment along the load direction, as observed here.
Lava eruption seems to have ceased in conjunction with this substantial collapse of the material, although minor changes prevailed near vent (c), possibly arising from drainage of lava already within the channel or slope instability.
We explain this phenomenon in terms of the inelastic collapse of granular materials.
This phenomenon could give rise to high crack growth rates and the abrupt collapse of the structural material.
No collapse of the shell materials occurred during the annealing process to remove the carbon cores.
The second method, limit state analysis, is based on a virtual work formulation to predict the collapse assuming the same set of material properties.
After calibrated based on the experimental results, the model was used to determine the collapse pressure as a function of material and geometric parameters of different pipes and defects.
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