1993
DOI: 10.1103/physrevlett.71.1593
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Cracklike surface instabilities in stressed solids

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Cited by 243 publications
(154 citation statements)
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“…[1][2][3][4] Many continuum models can be found in the literature on the surface morphological evolution under elastic effects, in which the surfaces are modeled as continuously changed profiles without any discrete structures on them. 2,[5][6][7][8][9][10][11][12][13][14][15][16] The stress in the solid is a destabilizing factor while the surface energy is a stabilizing one, and the planar surface of a stressed solid is unstable for perturbations with wave numbers less than a critical value. [6][7][8][9][10] These models work in the regime above the roughening transition temperature.…”
Section: Introductionmentioning
confidence: 99%
“…[1][2][3][4] Many continuum models can be found in the literature on the surface morphological evolution under elastic effects, in which the surfaces are modeled as continuously changed profiles without any discrete structures on them. 2,[5][6][7][8][9][10][11][12][13][14][15][16] The stress in the solid is a destabilizing factor while the surface energy is a stabilizing one, and the planar surface of a stressed solid is unstable for perturbations with wave numbers less than a critical value. [6][7][8][9][10] These models work in the regime above the roughening transition temperature.…”
Section: Introductionmentioning
confidence: 99%
“…The dynamics is ruled here by surface diffusion driven by the interplay between isotropic surface energy and elastic energy [12,13]. When the film is infinitely thick or when the substrate is infinitely rigid, different theoretical [14,15] and numerical [16,17,18,19] approaches revealed finite-time singularities enforced by elastic stress concentration which account for experiments in thick films [8,9] where dislocations can finally develop. However, these models can not describe experiments of thin films in the Stranski-Krastanov type of growth [5,6] where the surface organizes smoothly into islands separated by a wetting layer and evolving with a coarsening dynamics under annealing [6].…”
mentioning
confidence: 99%
“…By means of numerical approaches, it is possible to analyse more in general the evolution as in Refs. [112,113], where the formation of cusps separated by deep trenches was also linked to crack propagation. Several other studies are reported in literature (e.g.…”
Section: Non-linear Effectsmentioning
confidence: 99%