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Date: 28-2-2016
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Microscopic Approach
When a surface is created, the atomic planes near the surface are usually displaced. The direction and magnitude of this relaxation depends on the type of material and also the orientation of the surface. In rare gas crystals or ionic crystals, for example, the bonds between the atoms are relatively longrange. In the bulk, the relative position of the atoms is determined by the competition between the mutual repulsion of the nuclei and long-range forces (Coulombic in the case of ionic crystals). In this case, the atomic planes at the surface expand. In the case of face- or body-centered cubic metals, the situation is generally different: for close-packed planes without defects, a very small surface relaxation is generally observed. On the other hand, if a close-packed surface has a certain degree of roughness due to the presence of defects such as steps or islands, or if the surface is not close-packed, the outermost layer will relax considerably towards the core of the material, whilst certain layers further in will move toward the surface. As an example, Fig.1. shows the various motions of the (210) surface planes in platinum. These different relaxations compensate for the fact that the atoms at the surface have fewer near neighbours, whence the electron density is lower there. Relaxation is thus a way of compensating for changes in the electron density in each plane, in such a way as to make it as homogeneous as possible right out to the outermost surface.
Consider now a nanocrystal with approximately spherical shape. Relaxation of the first atomic planes will lead in this case to a pressure exerted by the surface on the core of the nanocrystal, and hence to an increase or a decrease in the lattice parameter. An effect is therefore induced not only by the adsorption state of the surface, but also by the surface itself. This effect is even more marked in semiconductors, where surfaces are generally reconstructed, in order to minimise the number of dangling bonds, which generates large stresses in the first layers.