The kinetics of silane pyrolysis on a silicon (111) surface has been investigated mass spectrometrically by molecular beam sampling over the silane pressure range
1×10−5 normalto 4×10−1
Torr and specimen temperature range 20°–1200°C. Silane decomposition was found to occur by the mechanism SiH4 )(normalgas→SiH4 )(normaladsorbed→normalSi+2H2 where both the amount of adsorbed silane and decomposition rate depend linearly on silane pressure. The activation energy for decomposition was
17±2 kcal mole−1
and the surface reaction efficiency (α) was found to obey the equation α=5.45exp)(−17×103/RT
At silane pressures
normalPs°false〉5×10−3 normalTorr
, small quantities of disilane formed by the bimolecular surface reaction SiH4)(normalads+SiH4)(normalads→Si2H6+H2 were detected with an activation energy for production of
56±6 kcal mole−1
.Measurements of silicon growth rate as a function of silane pressure supported the first‐order mechanism for decomposition. The condensation coefficient (σ) of silicon adatoms, determined from measurements of the silicon growth rate as a function of temperature and the surface reaction efficiency, was found to be less than 0.3 over the entire temperature range 700°–1200°C, indicating that the majority of silicon adatoms were desorbed. This behavior was accounted for on the basis of a step flow model for silicon growth and an activation energy for surface diffusion of
36±6 kcal mole−1
derived. Addition of arsine to the silane was found to inhibit silane pyrolysis. The measurements suggest an activation energy of
18±3 kcal mole−1
for desorption of arsenic adsorbed on the silicon (111) surface. Additions of more than 1% diborane to the silane, on the other hand, resulted in a significant increase in silane reaction efficiency.