Formation of Austenite Grain in Hypo-Peritectic Carbon Steels

The Minerals, Metals and Materials Society
Masayuki Kudoh Tohru Maruyama Yohichi. Ito
Organization:
The Minerals, Metals and Materials Society
Pages:
4
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1654 KB
Publication Date:
Jan 1, 2000

Abstract

When hypo-peritectic carbon steel is quenched during unidirectional solidification, the region of fine columnar grain is observed. It is classified into two coexisting phases. One is coexisting phases of liquid, delta and gamma in the upper part of the region, and the other is coexisting phases of delta and gamma in the lower part of the region. To form the coexisting part of the three phases means that solidification in this experiment proceeds in non-equilibrium state. The size of the narrow side of one fine columnar grain coincides with the arm spacing of a primary dendrite and this result is the same as the hyper-peritectic carbon steel. However, the boundary of the fine grain in the hypo-peritectic carbon steel is formed in different location from that of the hyper-peritectic carbon steel. The former is formed in the skeleton of the dendrite, while the latter is formed in the interspacing of the dendrite. The region of the fine grain changes suddenly to that of the coarse grain when the delta phase in the coexisting part of two phases disappears completely. Therefore, the delta phase in the hypo-peritectic carbon steel might prevent the growth of gamma grain. In order to recognize it, ferrite formers such as Mo, V and Ni are added in the sample. Then, the longitudinal length of the fine columnar grain extends in the sequence of the no addition, Mo, V and Nb.
Citation

APA: Masayuki Kudoh Tohru Maruyama Yohichi. Ito  (2000)  Formation of Austenite Grain in Hypo-Peritectic Carbon Steels

MLA: Masayuki Kudoh Tohru Maruyama Yohichi. Ito Formation of Austenite Grain in Hypo-Peritectic Carbon Steels. The Minerals, Metals and Materials Society, 2000.

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