arXiv · 0707.4082
Dewetting of a solid monolayer
Abstract
We report on the dewetting of a monolayer on a solid substrate, where mass transport occurs via surface diffusion. For a wide range of parameters, a labyrinthine pattern of bilayer islands is formed. An irreversible regime and a thermodynamic regime are identified. In both regimes, the velocity of a dewetting front, the wavelength of the bilayer island pattern, and the rate of nucleation of dewetted zones are obtained. We also point out the existence of a scaling behavior, which is analyzed by means of a geometrical model.
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Olivier Pierre-Louis, Anna Chame, Yukio Saito. 2007-07-27. Dewetting of a solid monolayer. https://doi.org/10.1103/physrevlett.99.136101
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