Presence of H2S in a carburizing, atmosphere causes S-adsorption which
retards carbon transfer and deposition and can suppress metal dusting
of iron and steels. In the latter process cementite Fe3C is an interm
ediate, graphite deposition would initiate its decomposition but graph
ite nucleation is prevented by adsorbed sulfur. Thus continued Fe3C gr
owth can be observed in the presence of H2S. Thermogravimetric studies
in CO-H-2-H2O-H2S mixtures have been con ducted at 500 degrees C at v
arious carbon activities a(C) and H2S/H-2-ratios. With increasing a(C)
higher H2S/H-2-ratios are needed to suppress metal dusting, with incr
easing H2S/H-2-ratio the kinetics of Fe3C growth change from diffusion
controlled parabolic kinetics to linear carbon transfer controlled ki
netics. At very high a(C) greater than or equal to 1000 besides Fe3C a
lso the Hagg carbide Fe5C2 was observed as an outer layer on the cemen
tite.