Abstract:Observations on the spatial distribution and on the strain dependence of the crack density are given for cracks formed during compressive, unidirectional, constantstrain-rate deform~tion of column~r-grain ice. Sp~fim~~s, in th~~~1in-size c;ange of a~out 2 9 mm, were stramed at the nom mal rates of 10 . ,10 and 10 . s at 10 C. The aXIsof hexagonal crystallographic symmetry of each specimen grain tended to be in the plane perpendicular to the long direction of the grains and to have a random orientation in that … Show more
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