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The corrosion of steels and of nickel‐based alloys was studied in exposure experiments at 600 °C beneath a molten CaSO4‐K2SO4‐Na2SO4‐PbSO4‐ZnSO4 sulphate mixture in N2‐5 vol.% O2 with and without additions of 1000 vppm HCl, 1000 vppm SO2 and 1000 vppm HCl in combination with 250 vppm SO2. In the N2‐5 vol.% O2 atmosphere, the corrosion products are iron‐ and nickel‐rich but chromium‐free precipitates of oxides in the solidified melt. Additionally, pits filled with layered corrosion products are formed, growing into the metal substrate. These layers consists of less soluble chromium‐rich oxides, containing varying amounts of zinc, (ZnCr2O4) alternating with potassium‐rich sulfates, most probably K2S2O7. The addition of 1000 vppm SO2 leads to a seperation of the melt in a K2S2O7 part close to the metal surface and a Ca‐rich part on top in contact with the gas atmosphere. Compared to the N2‐5 vol. % O2 atmosphere accelerated corrosion was observed. In the K2S2O7 part of the melt dissolved iron and nickel are identified, whereas in the Ca‐rich part iron‐ and nickel‐oxide precipitates are formed. Underneath the solidified salt, thin layers of sulfides are detected. In the N2‐5 vol.% O2‐1000 vppm HCl containing gas, the corrosive attack is also accelerated compared to the N2‐5 vol.% O2‐atmosphere. Much more oxide precipitates are found in the melt on every sample and the inward growth of the zinc‐free chromium‐rich oxides is significantly enhanced. Underneath the inward growing oxide small amounts of metal‐chlorides are detected. Compared to the SO2 containing gas, the corrosive attack is enhanced for the iron‐based materials, but retarded for the nickel‐based alloys. In the 1000 vppm HCl‐250 vppm SO2 containing gas, the corrosive attack is similar to the atmosphere containing only 1000 vppm HCl. In addition, sulfides are formed next to chlorides at the metal/scale interface.  相似文献   

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