1959
DOI: 10.1002/srin.195903079
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Die Verschiebung des Nonvarianzpunktes zwischen Eisen, Wüstit, Magnetit und Sauerstoff im System Eisen—Sauerstoff durch Legierungselemente oder fremde Oxyde, Auswirkungen auf das Verhalten von Eisenlegierungen beim Verzundern

Abstract: Zusammenhänge zwischen Temperatur der Wüstitbildung und Verzunderungsgeschwindigkeit von Eisen. Thermodynamische Betrachtungen über die Verschiebung der Bildungstemperatur des Wüstits beim Übergang m Dreistoffsysteme Eisen‐Sauerstoff‐Zusatzelement. Oxydationsversuche und mikroskopische Untersuchungen an Eisen‐Chrom‐, Eisen‐Nickel‐ und Eisen‐Mangan‐Legierungen. Erörterung der Versuchsergebnisse unter dem Gesichtspunkt der eingangs durchgeführten thermodynamischen Betrachtungen. Vorgang der inneren Oxydation von… Show more

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Cited by 8 publications
(3 citation statements)
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“…It appears that the magnetite nucleates preferentially. Brauns et al (19) showed that the temperature below which wustite formed in the scale increased as the Ni concentration increased: 21% Ni raised the temperature from 570 ~ to 680~ and this may indicate a tendency to form magnetite under conditions of rapid Ni enrichment. However, it appears likely that magnetite forms because it can dissolve up to 25% Ni whereas wustite can only dissolve a maximum of 0.84% (15).…”
Section: Eleetrochem Soe: S O L I D -S T a T E Sciencementioning
confidence: 99%
“…It appears that the magnetite nucleates preferentially. Brauns et al (19) showed that the temperature below which wustite formed in the scale increased as the Ni concentration increased: 21% Ni raised the temperature from 570 ~ to 680~ and this may indicate a tendency to form magnetite under conditions of rapid Ni enrichment. However, it appears likely that magnetite forms because it can dissolve up to 25% Ni whereas wustite can only dissolve a maximum of 0.84% (15).…”
Section: Eleetrochem Soe: S O L I D -S T a T E Sciencementioning
confidence: 99%
“…A further decrease in temperature below 570 • C leads to an unstable wuestite layer. Thus the oxide scale layer consists of two iron oxides, a thick layer of magnetite with about 80 wt %, and a thin haematite cover layer [10]. In the temperature range between 700 • C and 1250 • C, the oxide scale composition is nearly constant with a ratio of 1:4:95 for the layers of haematite, magnetite, and wuestite, respectively [11].…”
Section: Introductionmentioning
confidence: 99%
“…Because of the brittle nature of the scale, the sample preparation process for metallographic examination of the scale is difficult and time-consuming. 3,4) It was not uncommon in the open literature that some scale structures were presented with preparation damages, [5][6][7][8][9][10][11] which in some cases were treated as genuine porosities in the scales, and explained in great depths of their fundamental mechanisms of formation. 6,10) In many of these cases, it was either stated that the 'conventional method' was used for metallographic sample preparation, 5,11) or the metallographic preparation was conducted in 'the usual way'.…”
Section: Introductionmentioning
confidence: 99%