
AbstractThe hardness observations taken in the Canadian Snow Survey are analysed and found to depend on snow density, temperature, and crystal size. This strength property of the snow is found to be highly variable and the variability is attributed to unstable bonding between individual snow grains.
snow loads, charge de neige, propriété des matériaux, yield strength, properties of materials, résistance à la rupture, compression
snow loads, charge de neige, propriété des matériaux, yield strength, properties of materials, résistance à la rupture, compression
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