Abstract
The (111) cleavage in crystalline silicon was investigated by hybrid quantum/classical atomistic simulations showing that its remarkable stability is largely due to asymmetric -bonded reconstructions of the cleavage surfaces created by the advancing crack front. Further simulations show that the same reconstructions can induce an asymmetric dynamical response to added shear stress components. This explains why upward steps are much more common than downward steps on (111) cleavage surfaces, while “zigzag” cleavage with alternated (111) and facets will still occur in crystal samples fractured under [110] uniaxial loading.
- Received 7 June 2010
DOI:https://doi.org/10.1103/PhysRevLett.105.185502
© 2010 The American Physical Society