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Taylor and Francis Group, Philosophical Magazine Letters, 12(86), p. 763-771
DOI: 10.1080/09500830601023787
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Investigation of Newtonian creep in polycrystalline ice
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Abstract
The mechanism for Newtonian creep in polycrystalline ice has been studied. It is shown that the creep can be explained by dislocation glide along the basal plane with a constant dislocation density. The experimentally determined creep-rates agree well with the values calculated using Cole's constitutive model based on dislocation glide.