PART V - Partition of Alloying Elements Between Austenite and Proeutectoid Ferrite or Bainite

The American Institute of Mining, Metallurgical, and Petroleum Engineers
H. I. Aaronson H. A. Domian
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
16
File Size:
4478 KB
Publication Date:
Jan 1, 1967

Abstract

ELectvon-probe analgsis has been used to in7:estigatr the partition ot alloying- elements between aus-tenite and proeutectoid ferrite (or the Jerritic component of bainite) in high-purity Fe-C-X alloys, lsuully at tzco levels of carbon content fca 0.1 and 0.4 pct in ntost steels) at temperatures between the M, and the Ae3 in Si, mn, Ni, mo, Co, Al, Cr, Cu, and PI steels. No partition ous found during the early stages of transformation at any temperature studied in the Si, ,mo. Co, Al, Cr, and Cu steels. Partition did take place, Jrowel'er, in Ihe Mn, ATi, and Pt steels, occurring in lewtperature. regions below the Ae3 of ca 130°, 65", UNDERSTANDING the mechanisms through which alloying elements influence the kinetics of austenite decomposition reactions which proceed by nucleation and 35c respectively. A break was discovered in the TTT curve for the initiation oj the proeutectoid ferrite reaction in the latter steels at the temperature at which partition began. The alloy content in ferrite at the a:y bondavy remained at constart lecels, shown experimentally to be significantly above those corresponding to eqiilib+iu??l, e'en at the longest reaction times investigated (ca 1o6sec). The partition and the TTT curve observations foere rationalized on the basis of the thermodynamic treatment developed in an accompany ing paper. and diffusional growth has been a major research objective of physical metallurgy since the latter part of the 19th century. The measurements made on the dif-fusivities of carbon and of substitutional alloying elements in austenite during the 1930's and 1940's seemed to provide a useful clue as to the nature of these mechanisms. These measurements showed that the diffu-sivity of carbon is several orders of magnitude higher than that of the alloying elements at a given tempera-
Citation

APA: H. I. Aaronson H. A. Domian  (1967)  PART V - Partition of Alloying Elements Between Austenite and Proeutectoid Ferrite or Bainite

MLA: H. I. Aaronson H. A. Domian PART V - Partition of Alloying Elements Between Austenite and Proeutectoid Ferrite or Bainite. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1967.

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