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Kinetic Roughening of Fe/Fe(100) Epitaxial Thin Films

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We model kinetic roughening during Fe(100) homoepitaxy, where the formation of mounds with selected slope has been observed. Our model incorporates irreversible nucleation and growth of two-dimensional square islands in each layer, and a step-edge barrier to diffusive downward transport (which exceeds the barrier, Ed, to terrace diffusion by ESch). We estimate that ESch≈45meV compared with Ed≈450meV. To reproduce observed behavior, it is also essential for the model to incorporate "downward funneling" of depositing atoms to four-fold hollow adsorption sites, as this controls slope selection. Finally, we discuss model predictions for the non-monotonic temperature dependence of kinetic roughening.

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Bartelt, M., Evans, J. Kinetic Roughening of Fe/Fe(100) Epitaxial Thin Films. MRS Online Proceedings Library 399, 89 (1995). https://doi.org/10.1557/PROC-399-89

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