Trenches formed at Ge/Si(100) island bases become an effective strain-relie
f mechanism at high growth temperatures. Trenches result from diffusion of
the most highly strained material to regions of lower strain. The trench de
pth self-limits, scaling linearly with island diameter. A simple atomistic
model of island elasticity indicates that this self-limiting behavior is of
kinetic rather than energetic origin. (C) 2000 American Institute of Physi
cs. [S0003-6951(00)02224-5].