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- W2000783937 abstract "Concepts of dislocation micromechanics and of fracture mechanics have been used to derive a quantitative criterion for the brittle/ductile transition in polycrystalline ice under tension. The criterion is written in terms of a critical grain size dc, which is expressed as a function of both environmental parameters (temperature, strain rate) and material parameters (fracture toughness, lattice resistance to dislocation glide, grain boundary resistance to the propagation of slip). For d > dc the ice is considered to be brittle; for d < dc, it is ductile. While detailed experiments are needed to test the analysis, comparisons show reasonable agreement between theory and the limited data available." @default.
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- W2000783937 date "1979-11-01" @default.
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- W2000783937 title "An analysis of the brittle to ductile transition in polycrystalline ice under tension" @default.
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- W2000783937 doi "https://doi.org/10.1016/0165-232x(79)90001-6" @default.
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