Mc. Cheng et R. Chennupati, EVOLUTION OF NONEQUILIBRIUM ELECTRON-DISTRIBUTION FUNCTIONS AT HYDRODYNAMIC SCALES IN MULTI-VALLEY SEMICONDUCTORS, Journal of physics. D, Applied physics, 28(1), 1995, pp. 160-173
The concept of the physical evolution process for the distribution fun
ction is used to derive a non-equilibrium hydro-kinetic transport theo
ry. The hydro-kinetic distribution that is interpolated between the ki
netic and hydrodynamic levels is introduced to elucidate the physics o
f evolution for the distribution. The evolution scales of the distribu
tion are decomposed into characteristic scales of hydrodynamic paramet
ers, such as carrier density, energy and momentum characteristic times
. The coarseness of the hydro-kinetic distribution function is determi
ned by scales of the chosen hydrodynamic parameters. The hydro-kinetic
distribution is used to close the infinite set of moments and to dete
rmine the rate coefficients in the closed set of hydrodynamic equation
s. In this paper, the hydro-kinetic distribution at the energy charact
eristic scale is applied to study evolution of the electron energy/mom
entum distribution and transport parameters, including inter-valley tr
ansfer, in GaAs subjected to a fast varying electric field. Monte Carl
o (MC) simulations are also included to illustrate the difference betw
een evolution scales of the kinetic and tau(epsilon)-scale hydro-kinet
ic distributions. The study indicates that the electron distribution i
s strongly dependent on the mean energy but weakly on the average mome
ntum. In GaAs subjected to a rapid increase in field, effects of the m
omentum dependence is enhanced only near the peak of strong velocity o
vershoot, such as the overshoot in the Gamma valley. The Gamma-valley
energy scale hydro-kinetic (energy dependent) distribution thus apprec
iably deviates from the kinetic distribution near the peak of strong o
vershoot. As a result, the hydro-kinetic model leads to a smaller over
shoot in the Gamma valley than the Me method. In the case of less pron
ounced velocity overshoot, the energy scale hydro-kinetic distribution
can reasonably follow the evolution scale of the kinetic distribution
function.