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EnglishThis paper analyses the conditions for triggering of dry snow slab avalanches. As suggested by several Authors, we assume as a basic mechanism for avalanche triggering the mode II fracture of the weak layer lying beneath the stiff snow slab, i.e. we assume the presence of super-weak zones in the basal layer. By means of a linear elastic analysis, the shear stresses in the weak layer as well as the strain energy release rate caused by an increment of the super-weak zone are evaluated. Hence we introduce a stress failure criterion as well as an energy one. It is shown that the latter criterion can be seen as an extension of the criterion firstly proposed by McClung [McClung, D.M., 1979. Shear fracture precipitated by strain softening as a mechanism of dry slab avalanche release. Journal of Geophysical Research, 84(B7), 3519-3526.] for dry snow slab avalanche release. Finally we couple the two criteria, showing that the weak layer can fail only in a min–max band of thickness.
Triggering of dry snow slab avalanches: stress versus fracture mechanical approach / CHIAIA B.; CORNETTI P; FRIGO B. - In: COLD REGIONS SCIENCE AND TECHNOLOGY. - ISSN 0165-232X. - 53(2008), pp. 170-178.
| Titolo: | Triggering of dry snow slab avalanches: stress versus fracture mechanical approach |
| Autori: | |
| Data di pubblicazione: | 2008 |
| Rivista: | |
| Digital Object Identifier (DOI): | http://dx.doi.org/10.1016/j.coldregions.2007.08.003 |
| Appare nelle tipologie: | 1.1 Articolo in rivista |
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http://hdl.handle.net/11583/1822310
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