Hydrogen migration in solid-state crystallized and low-pressure chemic
al-vapor-deposited (LPCVD) polycrystalline silicon (poly-Si) was inves
tigated by deuterium diffusion experiments. The concentration profiles
of deuterium, introduced into the poly-Si samples either from a remot
e D plasma or from a deuterated amorphous-silicon layer, were measured
as a function of time and temperature. At high deuterium concentratio
ns the diffusion was dispersive depending on exposure time. The disper
sion is consistent with multiple trapping within a distribution of hop
ping barriers. The data can be explained by a two-level model used to
explain diffusion in hydrogenated amorphous silicon. The energy differ
ence between the transport level and the deuterium chemical potential
was found to be about 1.2-1.3 eV. The shallow levels for hydrogen trap
ping are about 0.5 eV below the transport level, while the deep levels
are about 1.5-1.7 eV below. The hydrogen chemical potential mu(H) dec
reases as the temperature increases. At lower concentrations, mu(H) wa
s found to depend markedly on the method used to prepare the poly-Si,
a result doe in part to the dependence of crystallite size on the depo
sition process. Clear evidence for deuterium deep traps was found only
in the solid-state crystallized material. The LPCVD-grown poly-Si, wi
th columnar grains extending through the film thickness, displayed lit
tle evidence of deep trapping, and exhibited enhanced D diffusion. Man
y concentration profiles in the columnar LPCVD material indicated comp
lex diffusion behavior, perhaps reflecting spatial variations of trap
densities, complex formation, and/or multiple transport paths. Many as
pects of the diffusion in poly-Si are consistent with diffusion data o
btained in amorphous silicon.