Joe Feldman (NRL), Jaro Fabian (formerly a PhD student at Stony Brook, now post-doc with Das Sarma at Maryland) and I have been studying the lattice vibrations of amorphous silicon using a realistic model of the atomic coordinates and the interatomic forces.
The picture above shows the vibrational densities of states of both crystalline and amorphous silicon. There is surprisingly little change when crystalline order is lost. However, the nature of the vibrational normal modes does change. The plot also shows the ``bond stretching character'' of each mode. Crystalline silicon has vibrations which can be classified by wavevector and by branch. Transverse branches involve atom motions perpendicular to the direction of propagation. These vibrations do not stretch the bonds very much. Longitudinal branches cause large stretches of bonds. In the low-frequency part of the spectrum, the crystalline modes clearly separate into these very different categories. The vibrational normal modes of amorphous silicon completely lose this differentiation. At a given frequency, all modes have the same ``bond stretching character.''
The next picture shows for the amorphous case how the vibrational amplitude of a given normal mode changes with distance as you go away from the atom with the largest vibrational displacement (for that branch.) Modes with frequency less than 72 meV extend throughout the material. The amplitude falls initially, but saturates at a constant value. Modes with frequency higher than 72 meV are localized. Their amplitudes fall off exponentially with distance. The frequency 72 meV which divides these two categories is called the mobility edge.
The picture above shows thermal conductivity measured on films of amorphous silicon in various laboratories around the world. In the temperature interval 10K < T < 20K the conductivity shows a "plateau" where it is nearly independent of temperature. Our theory shows that this plateau arises as a crossover from the low T regime where heat is carried by ballistically propagating long wavelength vibrational modes to the high T regime where heat is carried by modes which extend throughout the sample, but have no wavevector or group velocity. These modes have an intrinsically diffusive behavior. Wavepackets built from these modes spread diffusively (r^2 = 6Dt) with diffusivity D of order the Debye frequency times interatomic separation squared, or about 1 mm^2/s. These modes are not significantly populated until T > 20K, and then they begin to dominate the conductivity. We call these modes "diffusons."