Abstract
Three types of internal sulphidation (general internal, integranular) and a mixture of these occurred beneath relatively thick surface scales at low sulphur pressures where a noble metal sulphide is unstable. This critical sulphur pressure was higher when the surface sulphide scales were highly protective, as observed for FeCrAl and FeMn alloys sulphidized at intermediate sulphur pressures. Copious internal sulphidation was formed by sulphidation of FeMn, FeNi and NiCr alloys. For an Fe26.6 % Cr alloy the internal sulphidation occurred at 1173 K while it was confined along the grain boundaries at 1073 K. With increasing chromium content, a mixture of internal and intergranular sulphidation was formed at both temperatures. Austenitic stainless steels, SUS 316L and Incoloy 800, formed copious internal sulphidation at sulphur pressure of 10 −3.5 and 10 −3 Pa, and with decreasing sulphur pressures this changed rapidly to intergranular sulphidation. The usual internal sulphidation is explained by assuming an enhanced diffusion flux of sulphur due to the sulphur-metal interaction in the alloy phase, which has very low chemical diffusivity. For alloys with relatively high chemical diffusivity intergranular sulphidation takes place, because the metal-scale interface is unstable and the grain boundaries become inward protruding sites.
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