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Kinetics and mechanism of high-temperature sulfidation of an Fe-23. 4Cr-18. 6Al alloy in H[sub 2]S-H[sub 2] atmospheres

Journal Article · · Oxidation of Metals; (United States)
DOI:https://doi.org/10.1007/BF00665042· OSTI ID:6999937
 [1];  [2];  [3]
  1. Academy of Mining and Metallurgy, Krakow (Poland)
  2. Hokkaido Univ., Sapporo (Japan)
  3. McMaster Univ., Hamilton, Ontario (Canada)
Sulfidation of an Fe-23.4Cr-18.6Al (at.%) alloy was investigated in H[sub 2]S-H[sub 2] atmospheres, 10[sup [minus]6] [le] P[sub s[sub 2]] [le] 10[sub 2] Pa, at 973 K. It was found over this pressure range that sulfidation after an early transient period followed the parabolic rate law, being diffusion controlled. An investigation was carried out of the scales formed during early transient sulfidation over the sulfur pressure range p[sub s[sub 2]] = 10[sup [minus]6]-10[sup [minus]2] Pa. Fully developed scales were multilayered consisting of an inner compact layer of equiazed grains, an intermediate layer of equiazed and columnar grains exhibiting a small degree of porosity, and an outer porous layer of distinct plates and needles. The grains of the inner and intermediate layers contained quaternary sulfide phases. The plates and needles were composed of hexagonal (FeCr)Al[sub 2]S[sub 4] and (CrAlFe)[sub 2]S[sub 3] from which pyrrhotite, FeS, grew at p[sub s[sub 2]] [ge] 10[sup [minus]4] Pa. The alloy exhibited a small degree of internal sulfidation; the precipitates were Al[sub 2]S[sub 3] doped with Cr and Fe. Marker measurements indicated that growth of the inner sulfide layer was supported by inward migration of sulfur. The morphological development of the scales at 973 K was similar to that obtained at 1,073 and 1,173 K.
OSTI ID:
6999937
Journal Information:
Oxidation of Metals; (United States), Journal Name: Oxidation of Metals; (United States) Vol. 38:1-2; ISSN OXMEAF; ISSN 0030-770X
Country of Publication:
United States
Language:
English