2014
DOI: 10.1016/s1006-706x(14)60051-0
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Morphology of Oxide Scale and Oxidation Kinetics of Low Carbon Steel

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Cited by 34 publications
(18 citation statements)
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“…In general, the formation of the red scale is related not only to the content of Fe 2 SiO 4 , but also to its morphology and distribution. The formation mechanism of red scale has been reported in several studies [1][2][3][4][5][6][7][8]. Silicon reacts with oxygen diffusing into steel and precipitates as SiO 2 , which combines with FeO and then forms a separate phase called fayalite (Fe 2 SiO 4 ).…”
Section: Introductionmentioning
confidence: 99%
“…In general, the formation of the red scale is related not only to the content of Fe 2 SiO 4 , but also to its morphology and distribution. The formation mechanism of red scale has been reported in several studies [1][2][3][4][5][6][7][8]. Silicon reacts with oxygen diffusing into steel and precipitates as SiO 2 , which combines with FeO and then forms a separate phase called fayalite (Fe 2 SiO 4 ).…”
Section: Introductionmentioning
confidence: 99%
“…Fourthly, wustite occurs with a broad composition range that can be described as Fe 1´x O, with x varying from 0.04 to 0.17 [11]. The ion transport through oxides is dominated by the stoichiometry of the oxide (wustite) that is p-type [26,29].…”
Section: Oxidation Analysismentioning
confidence: 99%
“…Below 570˝C, only the last two layers are thermodynamically stable. Cao et al [11] investigated the isothermal oxidation kinetics of low carbon steel at temperatures ranging between 500˝C and 900˝C. They reported that the oxidation mass gain per unit area with time has a parabolic relation and that the oxidation rate decreases with time.…”
Section: Introductionmentioning
confidence: 99%
“…It has been reported that for pure iron, the initial oxidation rate in short times is determined by the chemical reactions between oxygen atoms at the surface of the metal and adsorbed oxidizing species . On the contrary, the diffusion of ionic species, such as oxygen, throughout the oxide layers is the rate controlling factor for the aforementioned phases …”
Section: Introductionmentioning
confidence: 99%
“…[8] On the contrary, the diffusion of ionic species, such as oxygen, throughout the oxide layers is the rate controlling factor for the aforementioned phases. [8,13] However, it has been reported that the growth rate of hematite depends on oxygen diffusion due to the abundance of oxygen close to the surface and that of wustite and magnetite mainly depends on the diffusion of cations, as they are closer to the base metal. [13,14] However, the growth mechanism for each of these three layers is still not well documented.…”
Section: Introductionmentioning
confidence: 99%