Abstract:This paper provides an elementary introduction to the basic concepts used in describing epitaxial crystal growth in terms of the thermodynamics and kinetics of atomic steps. Selected applications to morphological instabilities of stepped surfaces are reviewed, and some open problems are outlined. (2000). Primary 80A22; Secondary 35R35.
Mathematics Subject Classification
“…The exchange of atoms between the step and the surrounding terraces is another source of nonlocality in the motion of the steps, since it necessitates the solution of a moving boundary value problem for the concentration of adatoms on the terraces [2,8]. A particular case in this class of problems is the interior model for the electromigration of vacancy islands introduced in [12], and studied in detail in [16,24].…”
Section: Nonlocal Shape Evolution: Vacancy Islands With Terrace Diffumentioning
confidence: 99%
“…with appropriate boundary conditions at the step edge (see [8] for a general discussion). If the exchange of atoms with the step edge is rapid, so that thermal equilibrium is maintained at the boundary at all times, a circular stationary solution drifting at constant speed against the force direction can be found [12].…”
Section: Nonlocal Shape Evolution: Vacancy Islands With Terrace Diffumentioning
confidence: 99%
“…The equations of motion for the steps can be obtained from the solution of a one-dimensional moving boundary value problem for the adatom concentration on the terraces. This procedure has been reviewed in detail elsewhere [8]. Here we start the discussion directly from the nonlinear equations of motion, regarded as a (physically motivated) many-dimensional dynamical system.…”
Section: Step Bunching On Vicinal Surfacesmentioning
confidence: 99%
“…Comparison with (1.9) shows that f ± are linear functions with slopes γ ± , such that the stability condition reads γ + > γ − . In addition to the linear terms depending on the nearest neighbor step positions, (1.14) contains nonlinear next-nearest-neighbor contributions arising from repulsive thermodynamic step-step interactions of entropic and elastic origin [3,8], which drive the relaxation of the step train to its (equidistant) equilibrium shape. The sublimation rate for the model (1.14) is R = (γ + + γ − )l, hence for strongly conserved dynamics one has to set γ + = −γ − .…”
Section: Strongly and Weakly Conserved Step Dynamicsmentioning
confidence: 99%
“…The analysis of the nonlinear dynamics of step bunches is greatly simplified if it is possible to perform a continuum limit of the problem, thus passing from the discrete dynamical system (1.14) to a partial differential equation [8,47]. Coarse graining the discrete equations of motion (1.14), one arrives first at a "Lagrangian" continuum description for the step positions x i or the terrace sizes l i = x i+1 − x i by converting the layer index i into a continuous surface height h = ih 0 (here h 0 denotes the height of an elementary step) [43,48].…”
Section: Continuum Limit Traveling Waves and Scaling Lawsmentioning
“…The exchange of atoms between the step and the surrounding terraces is another source of nonlocality in the motion of the steps, since it necessitates the solution of a moving boundary value problem for the concentration of adatoms on the terraces [2,8]. A particular case in this class of problems is the interior model for the electromigration of vacancy islands introduced in [12], and studied in detail in [16,24].…”
Section: Nonlocal Shape Evolution: Vacancy Islands With Terrace Diffumentioning
confidence: 99%
“…with appropriate boundary conditions at the step edge (see [8] for a general discussion). If the exchange of atoms with the step edge is rapid, so that thermal equilibrium is maintained at the boundary at all times, a circular stationary solution drifting at constant speed against the force direction can be found [12].…”
Section: Nonlocal Shape Evolution: Vacancy Islands With Terrace Diffumentioning
confidence: 99%
“…The equations of motion for the steps can be obtained from the solution of a one-dimensional moving boundary value problem for the adatom concentration on the terraces. This procedure has been reviewed in detail elsewhere [8]. Here we start the discussion directly from the nonlinear equations of motion, regarded as a (physically motivated) many-dimensional dynamical system.…”
Section: Step Bunching On Vicinal Surfacesmentioning
confidence: 99%
“…Comparison with (1.9) shows that f ± are linear functions with slopes γ ± , such that the stability condition reads γ + > γ − . In addition to the linear terms depending on the nearest neighbor step positions, (1.14) contains nonlinear next-nearest-neighbor contributions arising from repulsive thermodynamic step-step interactions of entropic and elastic origin [3,8], which drive the relaxation of the step train to its (equidistant) equilibrium shape. The sublimation rate for the model (1.14) is R = (γ + + γ − )l, hence for strongly conserved dynamics one has to set γ + = −γ − .…”
Section: Strongly and Weakly Conserved Step Dynamicsmentioning
confidence: 99%
“…The analysis of the nonlinear dynamics of step bunches is greatly simplified if it is possible to perform a continuum limit of the problem, thus passing from the discrete dynamical system (1.14) to a partial differential equation [8,47]. Coarse graining the discrete equations of motion (1.14), one arrives first at a "Lagrangian" continuum description for the step positions x i or the terrace sizes l i = x i+1 − x i by converting the layer index i into a continuous surface height h = ih 0 (here h 0 denotes the height of an elementary step) [43,48].…”
Section: Continuum Limit Traveling Waves and Scaling Lawsmentioning
We present a quasi‐liquid mediated continuum model for ice growth consisting of partial differential equations informed by molecular dynamics simulations. The main insight from molecular dynamics is the appearance of periodic variations in the equilibrium vapor pressure and quasi‐liquid thickness of the ice/vapor interface. These variations are incorporated in the continuum model as subgrid scale microsurfaces. We show that persistent faceted ice growth in the presence of inhomogeneities in the ambient vapor field is due to a spontaneous narrowing of terraces at facet corners, which compensates for higher ambient water vapor density via feedback between surface supersaturation and quasi‐liquid thickness. We argue that this emergent behavior has the mathematical structure of a stable limit cycle and characterize its robustness in terms of ranges of parameters that support it. Because the model is relevant in the high‐surface‐coverage regime, it serves as a useful complement to the Burton‐Cabrera‐Frank framework. Quantitative aspects and limitations of the model are also discussed.
We consider the shape evolution of two-dimensional islands on a crystal surface in the regime where mass transport is exclusively along the island edge. A directed mass current due to surface electromigration causes the island to migrate in the direction of the force. Stationary shapes in the presence of an anisotropic edge mobility can be computed analytically when the capillary effects of the line tension of the island edge are neglected, and conditions for the existence of non-singular stationary shapes can be formulated. In particular, we analyse the dependence of the direction of island migration on the relative orientation of the electric field to the crystal anisotropy, and we show that no stationary shapes exist when the number of symmetry axes is odd. The full problem including line tension is solved by time-dependent numerical integration of the sharp-interface model. In addition to stationary shapes and shape instability leading to island breakup, we also find a regime where the shape displays periodic oscillations. (2000). Primary 53C44; Secondary 82C24.
Mathematics Subject Classification
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