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                           متالوژی:: 
                            سرعت اکسیداسیون
                        
                        Despite the rapid initial reactions, the longer-term oxidation rate of iron under isothermal-oxidation
Instead, the parabolic  oxidation rate constant decreased with time, which was attributed to the  formation of voids by the coalescence of vacancies at the scale-iron  interface.
As  will be discussed later, there exists a critical oxidizing gas flow rate at a  given oxidation temperature, below which the iron oxidation rate increases  with the gas flow rate, and above which the iron oxidation rate becomes  flow-rate independent.
The parabolic oxidation rate constants of cold-worked  samples at 400 to 550C are typically high initially, drop steeply after the  initial stages, and then approach constant values at longer oxidation  times.65,68 As in the case of oxidation at 580C and 600C, the scale struc  tures developed at 400 to 550C on cold-worked samples are more adherent  to the iron substrate, and more uniform in thickness, comprising a thin  hematite layer and a thick magnetite layer.65,68 More severe cold working  applied to the sample surface has been reported to result in more uniform,  thicker, and more adherent scale, together with a lower hematite-magnetite  thickness ratio The thickness ratios between the hematite and magnetite  layers developed at 500 to 550C on samples prepared by coarse mechanical  polishing or grinding were in the range 1:10 to 1:20.
The oxidation rates of annealed samples are typically much lower  and the parabolic rate constant decreases progressively with time due to the  gradual loss of contact between the scale and the iron substrate.69 The scales  are also nonuniform in thickness; at locations where the scale remains in  contact, it is relatively thick, whereas at locations where the scale-iron con  tact was lost, it is very thin.
 
                        
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