High-Temperature Atmospheric Corrosion of Fe-Cr-Si Alloys Studied by Mossbauer Spectroscopy

被引:9
作者
Idczak, Rafal [1 ,2 ]
机构
[1] Univ Wroclaw, Inst Expt Phys, Pl M Borna 9, PL-50204 Wroclaw, Poland
[2] Polish Acad Sci, Inst Low Temp & Struct Res, Ul Okolna 2, PL-50422 Wroclaw, Poland
关键词
atmospheric corrosion; high-temperature corrosion; iron alloys; Mossbauer spectroscopy; surface segregation; SURFACE SEGREGATION; MAGNETIC-PROPERTIES; OXIDATION; IRON; CHROMIUM; SILICON; MICROSTRUCTURE; EVOLUTION; ENTHALPY; BEHAVIOR;
D O I
10.5006/2776
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
The high-temperature atmospheric corrosion of iron-based Fe-Cr-Si alloys was studied using Fe-57 transmission Mossbauer spectroscopy (TMS) and conversion electron Mossbauer spectroscopy (CEMS). The Mossbauer measurements allow one to determine the chemical composition changes as well as the content of iron oxides in 300 nm subsurface layer and the bulk of studied samples during exposure to air at 870 K. The results indicate that the oxidation of iron atoms slows with increasing Si and Cr content in the specimens and as one could expect, the oxidation process in the bulk is much slower than in the 300 nm subsurface layer of studied materials. The parameters of the measured spectra made it possible to compute the iron oxidation kinetics. The comparison of the obtained kinetics for the Fe0.96Cr0.03Si0.01, Fe0.94Cr0.03Si0.03, and Fe0.90Cr0.05Si0.05 samples with corresponding data obtained previously for the binary Fe-Si and Fe-Cr alloys suggests that an addition of a relatively small amount of Cr to the dilute iron-based Fe-Si alloys has a negative effect on high-temperature corrosion resistance of the systems. At the same time, the present investigations show that the iron oxidation process is practically not observed when the alloy that is richer in Cr, Fe0.85Cr0.10Si0.05, is exposed to air at 870 K. Finally, the additional TMS measurements were performed for Fe0.85Cr0.10Si0.05 sample after exposure to air at 1,070 K and 1,270 K.
引用
收藏
页码:1083 / 1092
页数:10
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