Abstract
The energy stored in the elastic strain field of dislocations in hexagonal ice is calculated using anisotropic elasticity and the most complete set of elastic constants available. Ice is elastically fairly isotropic, and it is proposed that the high mobility of dislocations on the basal plane is due to dissociation of perfect dislocations on this plane.
Publisher
Canadian Science Publishing
Subject
General Physics and Astronomy
Cited by
11 articles.
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