The Crystallography and Nucleation of Pearlite

By choice of a suitable iron—manganese—carbon alloy it has been possible to study pearlite nodules growing in austenite, without the austenite transforming on cooling to room temperature. Thin foil electron microscopy has been used to examine the orientation relations between cementite, ferrite and...

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Veröffentlicht in:Proceedings of the Royal Society of London. Series A, Mathematical and physical sciences Mathematical and physical sciences, 1973-06, Vol.333 (1595), p.455-467
Hauptverfasser: Dippenaar, R. J., Honeycombe, Robert William Kerr
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container_title Proceedings of the Royal Society of London. Series A, Mathematical and physical sciences
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creator Dippenaar, R. J.
Honeycombe, Robert William Kerr
description By choice of a suitable iron—manganese—carbon alloy it has been possible to study pearlite nodules growing in austenite, without the austenite transforming on cooling to room temperature. Thin foil electron microscopy has been used to examine the orientation relations between cementite, ferrite and austenite as well as morphological aspects of the transformation. It is shown that one of the classical ferrite—cementite orientation relations found in pearlite (Pitsch—Petch) arises when the pearlite colonies nucleate on ‘clean’ austenite grain boundaries. The other familiar relation (Bagaryatski) arises when the colonies nucleate on pre-existing hyper-eutectoid cementite layers at the austenite grain boundaries. Some observations are made on the mode of nucleation of the pearlite nodules.
doi_str_mv 10.1098/rspa.1973.0073
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ispartof Proceedings of the Royal Society of London. Series A, Mathematical and physical sciences, 1973-06, Vol.333 (1595), p.455-467
issn 1364-5021
0080-4630
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language eng
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source JSTOR
subjects Alloys
Austenite
Ferrites
Grain boundaries
Iron
Nodules
Nucleation
Pearlite
Room temperature
Steels
title The Crystallography and Nucleation of Pearlite
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