Determination of diffusion coefficient of oxygen in ?-iron from internal oxidation measurements in Fe-Si alloys

1986 ◽  
Vol 21 (6) ◽  
pp. 2133-2137 ◽  
Author(s):  
Jun Takada ◽  
Masao Adachi
2004 ◽  
Vol 27 (2) ◽  
pp. 11233 ◽  
Author(s):  
L David Suits ◽  
TC Sheahan ◽  
AR Cabral ◽  
P Tremblay ◽  
G Lefebvre

2011 ◽  
Vol 696 ◽  
pp. 88-93 ◽  
Author(s):  
Shohei Nakakubo ◽  
Mikako Takeda ◽  
Takashi Onishi

The boundary constants between internal and external oxidation of Si or Cr containing steels (Fe-Si alloys or Fe-Cr alloys) at 850°C were calculated in order to clarify the formation mechanism of fayalite scale (Fe2SiO4) or chromite scale (FeCr2O4), which can form as a “sub-scale” in Si or Cr containing steels. The diffusion coefficient of oxygen in the alloy, Do, and the oxygen concentration at the specimen surface, NO(s), which are constituents of the internal oxidation rate constant, (2DONO(s)/NB(O)n), were calculated for various oxidation conditions, and the rate equation for internal oxidation was derived. By comparing the calculated and measured values of (2DONO(s)/NB(O)n), we confirmed that the rate equation determined for internal oxidation was reasonable. The boundary condition between internal and external oxidation of Si or Cr containing steels (Fe-Si alloys or Fe-Cr alloys) at 850°C were also calculated by substituting the calculated values of DO and NO(s) into the rate equation.


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