A damped Kuramoto–Sivashinsky equation describing the deviation of an interface
from its mean planar position during normal-incidence ion-sputtered erosion of a
semiconductor or metallic solid surface is derived and the magnitude of the gradient
in its source term is approximated so that it will be of a modified Swift–Hohenberg
form. Next, one-dimensional longitudinal and two-dimensional rhombic planform
nonlinear stability analyses of the zero deviation solution to this equation are
performed, the former being a special case of the latter. The predicted theoretical
morphological stability results of these analyses are then shown to be in very good
qualitative and quantitative agreement with relevant experimental evidence
involving the occurrence of smooth surfaces, ripples, checkerboard arrays of pits,
and uniform distributions of islands or holes once the concept of lower- and
higher-threshold rhombic patterns is introduced based on the mean interfacial
position.
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