Nanometer ripple formation and self-affine roughening of ion-beam-eroded graphite surfaces

Citation
S. Habenicht et al., Nanometer ripple formation and self-affine roughening of ion-beam-eroded graphite surfaces, PHYS REV B, 60(4), 1999, pp. R2200-R2203
Citations number
27
Categorie Soggetti
Apllied Physucs/Condensed Matter/Materiales Science
Journal title
PHYSICAL REVIEW B-CONDENSED MATTER
ISSN journal
01631829 → ACNP
Volume
60
Issue
4
Year of publication
1999
Pages
R2200 - R2203
Database
ISI
SICI code
0163-1829(19990715)60:4<R2200:NRFASR>2.0.ZU;2-C
Abstract
The topography of (0001)-graphite (highly oriented pyrolytic graphite) surf aces eroded by a 5 keV Xe+ ion beam has been investigated using scanning tu nneling microscopy. For tilted incidence of the ion beam and ion fluences o f about 10(17) cm(-2), a quasiperiodic ripple topography with characteristi c wavelengths between 40 and 70 nm has been found. As predicted by continuu m theory and Monte Carlo simulations, below a critical angle theta(C) the r ipples are oriented perpendicular to the ion beam projection onto the surfa ce, while for angles above theta(C) the ripple orientation is parallel to t he ion beam projection. The critical angle theta(C) lies between 60 degrees and 70 degrees, in agreement with the predictions of the continuum theory. For rising ion fluences, large scale perturbations of the surface topograp hy occur indicating a nonlinear behavior governed by the Kardar-Parisi-Zhan g universality class. [S0163-1829(99)50628-0].