摘要

The theory of residually stressed crystals is discussed in the context of the finite deformation theory of elastic-plastic solids. Here residual stress is assumed to be due to the prior plastic flow of a single crystal. On the basis of recent experiments, as well as the structure of the underlying theory, we advance the view that the lattice orientation field should be regarded as data. This stands in contrast to the classical theory in which dislocation density is assigned.

  • 出版日期2012-10