Abstract

Using the three-dimensional Monte Carlo model, the effect of monovacancies on the diffusion exchange between the steps on the (111) surface of a diamond-like crystal during sublimation was investigated. The critical terrace width L cr (the distance from the step edge to the nearest stable vacancy islands) was determined as a function of the relationship between the energy of adatom formation at the smooth terrace E n and the energy of adatom desorption from the terrace E d with retention of the sum of these energies E sub=E n+E d, which characterizes the sublimation of a substance. A well-pronounced maximum exists in the dependences L cr(E n) obtained. The formula is suggested which well describes the dependences L cr(E n) for various values of E sub. The extrapolation of the dependence L cr(E n) to the value E sub=4.2 eV, which is characteristic of Si, permits us to compare the model results with the experimental data of other authors. The explanation of a threefold increase in the terrace width, which is observed experimentally at about 1500 K, is suggested.

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