Abstract
The evolution of Si(100) surfaces has been studied during oblique high-fluence ion sputtering by means of atomic force microscopy. The observed surface morphology is dominated by nanoscale ripples and kinetic roughening at small and large lateral scales, respectively. The large-scale morphology exhibits anisotropic scaling at high fluences with different roughness exponents and in the directions normal and parallel to the incident ion beam, respectively. Comparison to the predictions of single field and two-field (“hydrodynamic”) models of ion erosion suggests the relevance of nonlinearities that are not considered in the simpler anisotropic Kuramoto-Sivashinsky equation.
- Received 9 January 2009
DOI:https://doi.org/10.1103/PhysRevB.79.115437
©2009 American Physical Society