4/26/2002, Friday Evolution of Surface Roughness

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Presentation transcript:

4/26/2002, Friday Evolution of Surface Roughness

Model

Chemical Potential for Roughness Evolution

Interface Energy Change Thickness = t g: solid-etchant interface energy density Curvature

Strain Energy Change Strain energy difference w0 is the strain energy of flat surface

Etching Rate g: solid-etchant interface energy density Curvature Strain energy difference w0 is the strain energy of flat surface

Competition of Two Tendencies Surface energy g For a perfectly flat surface, a stress applied parallel to the surface induces a uniform stress state in the solid. For a wavy surface, however, the stress field is nonuniform: the magnitude of the stress is larger at troughs than at crests. Consequently, the solid evaporates faster at the troughs than at the crests, so that the wave amplitude grows over time, and the surface roughens. When both surface energy and stress act together, the ratio of the surface energy to the elastic energy defines a length scale: short waves decay, but long waves grow. Residual stresss

Interface Energy Influence on Roughness Evolution For a perfectly flat surface, a stress applied parallel to the surface induces a uniform stress state in the solid. For a wavy surface, however, the stress field is nonuniform: the magnitude of the stress is larger at troughs than at crests. Consequently, the solid evaporates faster at the troughs than at the crests, so that the wave amplitude grows over time, and the surface roughens. When both surface energy and stress act together, the ratio of the surface energy to the elastic energy defines a length scale: short waves decay, but long waves grow. Surface energy g 

Strain Energy Influence on Roughness Evolution For a perfectly flat surface, a stress applied parallel to the surface induces a uniform stress state in the solid. For a wavy surface, however, the stress field is nonuniform: the magnitude of the stress is larger at troughs than at crests. Consequently, the solid evaporates faster at the troughs than at the crests, so that the wave amplitude grows over time, and the surface roughens. When both surface energy and stress act together, the ratio of the surface energy to the elastic energy defines a length scale: short waves decay, but long waves grow. Residual stresss 

Frequency Dependency of Interface Energy Change

Frequency Dependency of Strain Energy Change

Frequency Dependency of Etching Rate

Roughness Evolution Pattern Stress state: Material parameters: