1. Energetics of steps and reconstructed terraces of a two-dimensional semi-infinite solid
- Author
-
R. Arief Budiman
- Subjects
geography ,geography.geographical_feature_category ,Acoustics and Ultrasonics ,Chemistry ,Elastic energy ,Geometry ,Condensed Matter Physics ,Surfaces, Coatings and Films ,Electronic, Optical and Magnetic Materials ,Stress (mechanics) ,Stress field ,Surface tension ,Condensed Matter::Materials Science ,Classical mechanics ,Terrace (geology) ,Vicinal ,Surface reconstruction ,Plane stress - Abstract
Stress and displacement fields of a two-dimensional solid under plane strain are solved subject to surface reconstruction boundary conditions. The alternating lateral Dirac-δ forces at steps owing to the reconstruction obtained by Alerhand et al (1988 Phys. Rev. Lett. 61 1973–6) are recovered from the gradient of the stress field solution. Sinusoidal vertical and lateral displacements on a terrace are obtained, in addition to the vertical force distribution, in the direction normal to the surface. Reconstructed periodic terraces reduce their elastic energy by increasing their average width, but the elastic energy density reaches a finite limit with an increased terrace width. A like-oriented step–step interaction with the force dipole from the surface reconstruction, using the Marchenko–Parshin model, is considered and found to be repulsive. Reconstructed terraces of a vicinal surface are thermodynamically stable when the surface has a large dangling bond energy and a large miscut angle. Small miscut angle or small surface tension tends to destabilize the surface, although our result suggests that a multilayer configuration will metastabilize the terraces owing to the interface elastic mismatch.
- Published
- 2005
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