Conclusions
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1.
Carbon increases the stability of the austenite in the transition zone; in welded samples of base metal containing 0.01 and 0.18% C the austenite in the base metal decomposes with formation of a structure corresponding to that resulting from quenching.
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2.
Carbides are formed from austenite and alloyed martensite in the transition zone during isothermal heating at temperatures ensuring high diffusional mobility of carbon atoms and carbide-forming elements. The precipitation of carbon from the austenite and martensite lattices during crystallization of the carbide phase favors pearlitic and intermediate transformation of these phases.
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Literature cited
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Additional information
Translated from Metallovedenie i Termicheskaya Obrabotka Metallov, No. 6, pp. 48–50, June, 1964
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Yarkovoi, V.S., Ivanov, V.D. Structure of the transition zone in weld seams of different steels welded together. Met Sci Heat Treat 6, 382–384 (1964). https://doi.org/10.1007/BF00775337
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DOI: https://doi.org/10.1007/BF00775337