The time and temperature dependence of hydrogen permeation through sil
icon oxide into polycrystalline silicon was examined. The presence of
an oxide layer causes the H flux into the underlying polycrystalline s
ilicon (poly-Si) to decrease by more than 4 orders of magnitude compar
ed to poly-Si without an oxide layer. For oxides thicker than 0.1 mu m
the H flux is independent of the hydrogenation time. On the other han
d, a direct exposure of poly-Si to monatomic H exhibits a power-law de
crease in H flux with time. Without the presence of an oxide layer the
H flux exhibits a weak temperature dependence and is activated with E
(A) = 0.31 eV. The activation energy does not change significantly whe
n diffusing through an oxide, indicating that an increase in barrier h
eight cannot account for the striking decrease in H flux. The implicat
ions of these results for H diffusion are discussed.